中国水土保持科学
中国水土保持科学
 
 
 
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2020 Vol.18 No.2  Published 2020-04-30
  
 
Yellow River Basin
1 ZHOU Wenjie, WEI Tianxing, LIU Guangquan, ZHU Qingke
Coupling relationship between Hippophae rhamnoides community and soil factor in typical returning farmland to forest area in northern Shaanxi province
[Background] As a pioneer species of soil and water conservation forests, Hippophae rhamnoides is widely planted in the water-wind erosion interlaced region of the Loess Plateau. Information on its adaptability and effects on soils is valuable for the management of forest land in this area. The growth and development of H. rhamnoides may change soil physical and chemical properties which will affect the plant growth as a feedback. That is, there may be a certain coupling relationship between soil and vegetation. Studying the coupling relationship between soil and H.rhammoides may provide a theoretical basis for the sustainable management of H. rhamnoides forest.[Methods] Based on the soil physiochemical properties and growth status of vegetation of H. rhamnoides community in typical converting farmland to forest area in Wuqi county, Shaanxi province, variance analysis method was used to determine the differences in soil physical and chemical properties among different soil depths, stand types and slope aspects. Principal component analysis was used to compare the differences in soil physical and chemical properties of different stand types of H. rhamnoides. The gray correlation model was used to analyze the correlation between soil factors and tree height, basal diameter of H. rhamnoides and herb layer biomass under H. rhamnoides forest.[Results] 1) The soil physical and chemical properties of H. rhamnoides community varied significantly in different soil depths. Stand type and aspects had significantly interactive effect on soil total nitrogen and capillary porosity. Soil total nitrogen and capillary porosity of the Pinus tabuliformis+H. rhamnoides on sunny slope were significantly higher than those on shady slope and other stand types. 2) Soil organic matter, total nitrogen and capillary porosity were the dominant factors reflecting the soil physical and chemical properties. The pure H. rhamnoides forest on shady slope and the Pinus tabuliformis+H. rhamnoides on sunny slope exhibited higher soil improvement. 3) The order of average gray correlation degree between the H. rhamnoides community and soil factors was capillary porosity > total nitrogen > organic matter > non-capillary porosity > available phosphorus > soil density > available potassium.[Conculsions] There is a strong mutual promotion between the growth of vegetation in H. rhamnoides community and the improvement of soil physical and chemical properties. Therefore, H. rhamnoides is suitable for being planted in the loess area of northern Shaanxi. In order to promote the improvement of soil by H. rhamnoides to achieve the purpose of vegetation succession, the pure H. rhamnoides forest on sunny slope is suggested as the transformation of Pinus tabuliformis+H. rhamnoides, while the pure H. rhamnoides forest is more suitable for shady slope.
2020 Vol. 18 (2): 1-9 [Abstract] ( 561 ) [HTML 1KB] [PDF 1005KB] ( 648 )
10 BAI Limin, YU Xiaojie, QI Yanbing, WU Juan, YANG Yuchun
Spatio-temporal variation of NDVI and its quantitative relationship with environmental factors in Shaanxi province
[Background] Vegetation and its changes are not only important metrics for the effects of regional climate and human factors on the environment but are also of great importance to hydrological, ecological and global changes. Vegetation coverage change is a synergic result of environmental impacts, and it can be considered as an important basis for regionally ecological environment and soil erosion monitoring. Shaanxi is one of the earliest provinces implementing the Grain for Green Project (GGP). The analysis of spatio-temporal variation of NDVI and its quantitative relationship with environmental factors is an effective way to evaluate the benefits of GGP on soil and water conservation in the past 20 years.[Methods] Based on the data of MODIS NDVI, this study carried out the temporal and spatial variation characteristics of NDVI in long time series (2000-2016) and multi-period phase (year, season and month) since the application of GGP in Shaanxi province, and the quantitative analysis of the contribution of each factor using RDA method was conducted.[Results] 1) The spatial variation of NDVI in Shaanxi province gradually decreased from south to north. The average NDVI ranged from 0.80 to 0.93 in Qinba mountain area, and ranged from 0.60 to 0.80 in Guanzhong plain area as well as it ranged from 0.40 to 0.60 in the Loess Plateau area. From 2000 to 2016, the average annual value of NDVI fluctuant increased from 0.41 to 0.51 with the 25.8% increment in the whole Shaanxi province. 2) Specially, timely NDVI increment and the coefficient variation (CV) showed as Loess Plateau > Guanzhong plain > Qinba mountain area, which was consistent with the implement area of GGP mostly distributed in the Loess Plateau area. 3) Seasonally, the highest NDVI was in the summer with the average NDVI value of 0.66, followed by autumn and spring, and the lowest was in winter with an average NDVI value of 0.32. Due to vegetation change over seasons, the photosynthetic rate of vegetation was higher in July and August, and the peak of NDVI appeared in this period. 4) In the first half year, NDVI showed a monthly increasing trend, and reversed in the second half year. The spatial and temporal variation of NDVI was the result of the synthesized influence of multi-dimensional factors such as geographical location, climate, and topography. The total interpretation ability of environmental factors to NDVI variation reached 62%, among which the factors that had significant influence on NDVI variability were precipitation, latitude, slope and air temperature, the interpretation degree was 28.34%, 28.12%, 23.83% and 9.44%, respectively.[Conclusions] The implement of the GGP project has significantly increased the vegetation coverage in the past 16 years which is evidently beneficial to the soil and water conservation. And the natural factors are responsible for the spatial variation and anthropogenic factors are responsible for the temporal variation.
2020 Vol. 18 (2): 10-18 [Abstract] ( 545 ) [HTML 1KB] [PDF 6179KB] ( 463 )
19 LI Jing, MA Li
Coupling relationship between land use changes and its eco-environmental effect in Yanchi county
[Background] With the rapid development of social economy, human's wrong behavior in the upper and middle reaches of the Yellow River has seriously negatively affected the high-quality development of the river basin and restricted the local people to get rid of poverty. Yanchi county of Ningxia Hui Autonomous Region is located in the Yellow River basin typical agricultural and pastoral ecotone. Therefore, to discuss the coupling relationship between land use changes and its eco-environmental effects in Yanchi county not only will be quite helpful for the scientific decision-making of correct human behavior but also provide guidance for the ecological protection and high-quality development in the whole Yellow River basin.[Methods] In this study, Yanchi county was selected as a case study region, based on the land use data of 3 periods including 2005, 2010 and 2015, respectively, the land use change, ecological environment indexes and landscape indexes of Yanchi county were analyzed deeply through dynamic attitude, transfer matrix and ecological environment quality index.[Results] The change rate of comprehensive land use of Yanchi from 2005 to 2010 was 0.205%, and that from 2010 to 2015 was 0.814%. The change rate of comprehensive land use from 2010 to 2015 was 0.609% higher than that of the previous five years. The grassland and unutilized land in Yanchi county decreased from 465 600 hm2 to 454 300 hm2 with a decrease rate of 2.43% from 2005 to 2015, while arable land, woodland and residential land continuously increased from 11 100 hm2 to 22 500 hm2 with a growth rate of 102.7%. The area of unutilized land was decreasing, arable land and woodland were increasing. The comprehensive annual change rate of land use type and the comprehensive index of ecological environment continuously increased. During the ten years period, the contribution rate of grassland to the environmental quality has decreased. Landscape diversity showed a continuous growth trend, from 1.087 to 1.138; the dominance index showed a continuous rise trend, from 0.606 to 0.635. The landscape gradually developed to a reasonable direction. The intensity of human interference in the process of landscape evolution is effectively controlled, and the living environment of human settlements is gradually improved, and human protection of the natural environment exceeded its destruction.[Conculsions] It could be concluded explicitly, for the same or similar areas as Yanchi in the Yellow River basin, scientific and rational land use should be combined with local development planning, strengthen ecological protection, according to the concentrated development, stable through the land use dynamic change, this research also implicated a successful example to realize the rational utilization of water and soil resources and high quality development synchronously.
2020 Vol. 18 (2): 19-25 [Abstract] ( 617 ) [HTML 1KB] [PDF 2403KB] ( 444 )
26 ZHANG Peng, WANG Dongmei, HE Kangning, LI Ping
Site type division and optimal vegetation allocation in small watershed in the Loess Plateau-Tibetan Plateau transition zone
[Background] The Loess Plateau-Tibet Plateau transition zone is the most vulnerable and fastest-changing region in the world ecological environment. The local land degradation is serious, and the plantations after returning farmland to forest generally have a single stand and an excessive density. How to optimize vegetation within a small watershed, and how to optimize vegetation has become an essential issue. The purpose of this article is to explore the division of site types in the transition zone and the vegetation optimization models under each site type.[Methods] This study focused on the small watershed of Anmen Beach. Forty typical sample plots were selected in the watershed. The slope and slope of each plot were measured using a handheld compass, and the longitude, latitude, and altitude of each plot were determined using handheld GPS. The vegetation types of each plot were recorded. After digging the soil profile in each site, the original soil samples were taken in layers using a ring knife with a volume of 100 cm3. Each sample was repeated three times. The soil bulk density and moisture were obtained by drying. Factors such as altitude, slope, aspect, slope position, soil bulk density, soil moisture, and vegetation type were summarized as indexes for 40 sample plots. Cluster analysis was used to summarize and classify plots in small watersheds to obtain site type classification. Principal component analysis was used to obtain the variance contribution of the main factors and determine the dominant factors.[Results] 1) When the clustering coefficient is 6 and the number of categories is 5, the clustering coefficient curve becomes noticeably slower, and 40 plots are divided into 5 categories:Low altitude sunny and gentle slope site (T1), low altitude shady and steep slope site (T2), low altitude shady slope site (T3), medium altitude shady and gentle slope site (T4), and high altitude shade and steep slope (T5). 2) The first three principal components by the principal component analysis have synthesized 68.484% of all the information. The three principal component principal factors are altitude, slope, and aspect, and the coefficients are -0.687, 0.696, and 0.744, respectively. And we speculate that soil moisture is a potential dominant factor affecting site type division.[Conculsions] In site type (T1), the pure forest of Pinus tabuliformis and Juniperus przewalskii should be optimized as mixed forest by adding Caragana korshinskii and other shrubs. Site type (T2) mixed forest of Populus cathayana and Larix principis-rupprechtii should be selectively cut and Picea crassifolia seedlings should be replanted. In the site types (T2 and T3), the pure forests of L. principis-rupprechtii and Betula platyphylla in North China should be subjected to proper thinning, followed by P. crassifolia replacement to accelerate the natural succession. Site type (T3 and T4) should be in appropriate thinning P. crassifolia pure forest to expand the forest window.
2020 Vol. 18 (2): 26-35 [Abstract] ( 535 ) [HTML 1KB] [PDF 863KB] ( 512 )
 
Foundamental Studies
36 TANG Chongjun, LIU Yu, XU Aizhen, GUO Liping
Effect assessment of land cover pattern on soil and water loss on red soil plots
[Background] Evaluating the potential of spatial pattern of land cover on preventing soil and water loss by field monitoring is time-consuming and financially expensive. Pattern indices designed with concern of soil erosion, sediment flow and hydrological processes provide time-saving and low-cost solution. However, most of these indices are developed, tested and applied in arid and semiarid environment. Their suitability in areas covered by red soil and with greater precipitation is untested.[Methods] In this paper, the Directional Leakiness Index (DLI) and Flow-length-weighted Directional Leakiness Index (FDLI) were applied to assess the soil and water retention capacity of land cover patterns at plot scale in humid climate and with red soil. Runoff generation and sediment yield of ten 20m-by-5m plots (coded as PG1-PG10) with different land cover patterns were compared and used to test suitability of these two indices.[Results] The plots with grass bands paralleling to elevation contours have low DLI and FDLI compared with those without grass strips. The plots can be ranked differently according to runoff depth and sediment yield. According to runoff depth, the ten plots are ranked as PG4 > PG10 > PG9 > PG8 > PG1 > PG3 > PG6 > PG7 > PG2 > PG5. When ranked based on sediment yield, these plots are ranked as PG9 > PG10 > PG8 > PG4 > 2 > PG3 > PG1 > PG6 > PG7 > PG5. It is showed that DLI is logarithmically related with sediment production and runoff depth. Significant logarithmic regressions also are derived between FDLI and sediment yield, and between FDLI and runoff depth. The goodness of regression equations between land cover pattern indices and sediment yields (R2=0.771 6 for DLI, R2=0.890 7 for FDLI) is better than that of regression equations between land cover pattern indices and runoff depths (R2=0.598 7 for DLI, R2=0.684 7 for FDLI). For plots with a strong soil and water retention capacity, and accordingly lower DLI and FDLI, the responses of sediment yield and runoff generation to rainfall depth can be described by linear or exponential equations. However, for plots that have low capacity to retain soil and water, i.e., with great DLI and FDLI, the goodness of both linear and exponential regression equations between runoff depth and rainfall depths and between sediment yield and rainfall depth are close to zero, which argues that both linear equation and exponential equation are unsuitable for describing the response of runoff generation and sediment yield to rainfall depth.[Conculsions] These results confirmed the suitability of DLI and FDLI for ranking a set of land cover patterns according to capacity in soil and water loss prevention, and the importance of vegetation cover pattern for soil and water conservation in this humid and red soil covered region. It is also emphasized that reclassifying land cover into sources and sinks according to their actual effect on sediment yield and runoff generation is necessary, which can evidently promoted the effectiveness of the indices used to coupling the land cover pattern with soil loss and runoff generation.
2020 Vol. 18 (2): 36-42 [Abstract] ( 566 ) [HTML 1KB] [PDF 2821KB] ( 485 )
43 YUE Tongjia, ZHANG Shouhong
Impacts of rainfall change on water saving and runoff control performance of rainwater harvesting systems
[Background] Rainwater harvesting, as one of the important soil and water conservation measures to alleviate shortage of water resources and to relieve pressures on water supply and drainage systems in urban areas, has been increasingly used as an effective practice for the Sponge City and Water Saving City construction. Design and construction of rainwater harvesting systems should meet future water demand scenarios and rainfall conditions, however, most of current studies of rainwater harvesting systems use only historical climate and water demand data. Rainwater harvesting systems designed with historical data may not be able to sustainably meet water saving or stormwater management requirements under future climate conditions.[Methods] In this study, the plausible impacts of rainfall change on water saving and stormwater management performance of rainwater harvesting systems were investigated by comparing the water supply reliability (g), tap water saving efficiency (w) and runoff reduction efficiency (η) of rainwater harvesting systems in Fuzhou and Urumqi calculated using the future (2020-2050) and historical (1985-2015) daily rainfall time series. A downscaling technique based on linear and nonlinear regression analysis and the CLIGEN model was evaluated and employed to generate the future daily rainfall with the projections of 21 Global Circulation Models. A daily water balance model was developed to simulate the hydrologic operation of rainwater harvesting systems. Toilet flushing water demand was considered in this investigation.[Results] The simulated rainfall data of Fuzhou and Urumqi from 1960 to 2005 using the regression analysis for spatial downscaling and the CLIGEN model for temporal downscaling is close to the measured rainfall data. The downscaling technique performs well in simulating the occurrence of daily rainfall at both of the cities. Therefore, the CLIGEN model could alternatively be used at Fuzhou and Urumqi for rainwater harvesting system analysis. The downscaling rainfall data shows that mean annual rainfall in Fuzhou and Urumqi in 2020-2050 is going to increase by 2.67% and 28.23% compared with that in 1985-2015, respectively. The water saving performance of rainwater harvesting systems is positively affected by the increases in future rainfall, as rainwater harvesting systems with smaller tank sizes and/or smaller catchment areas could supply adequate water for demand at a desired tap water saving efficiency or water supply reliability. The stormwater management performance, however, is negatively affected under the conditions of future rainfall change, as a larger tank size or larger catchment area is required to achieve desired runoff reduction efficiency.[Conculsions] The responses of water saving and stormwater management performance of rainwater harvesting systems to rainfall change are varying with not only the system dimensions (i.e., storage capacity and catchment area), but also locations with different rainfall conditions. Rainwater harvesting systems in a drier city with less rainfall are more sensitive to rainfall change. Rainwater harvesting systems with larger storage capacity and/or larger catchment area are expected to be more resilient to rainfall change. Therefore, the ability of rainwater harvesting systems to adapt to rainfall change could be increased by designing larger reservoirs and catchment areas.
2020 Vol. 18 (2): 43-51 [Abstract] ( 405 ) [HTML 1KB] [PDF 3820KB] ( 428 )
52 JIANG Chunxiao, WANG Bin, WANG Yujie, WANG Yunqi, HU Bo, ZHANG Wenlong
Soil aggregate stability of typical forest stands in the Jinyun Mountain based on Le Bissonnais method
[Background] The slope land of yellow soil is one of the main source of soil erosion for the middle and upper reaches of the Yangtze River, while there is still a research gap in soil aggregate stability under typical forests in the yellow soil area. When using aggregate stability to assess soil erodibility, samples are usually collected from 0-20 cm soil layer. However, the surface of soil (0-1 cm) is still the active layer where various activities act although there is no obvious crust in forest land. Compared with the study on 0-20 cm soil layer, it is important to clarify the aggregate stability of the very surface layer for forest soil.[Methods] Mixed coniferous and broad-leaved forest, evergreen broad-leaved forest, Phyllostachys pubescens forest and shrub forest in the Jinyun Mountain were selected as research sites. In each site, 5 m x 20 m plots were selected. Samples were collected from the surface soil (0-1 cm) and subsoil (>1-20 cm), and 3 repeats along diagonal of each plot and mixed for each plot. The aggregate breakdown mechanism was distinguished by fast wetting test (FW), slow wetting test (SW) and stirring test (ST) in the Le Bissonnais (LB) method, and their stability was expressed by MWD (mean weight diameter)FW, MWDSW, and MWDST, respectively. Soil properties such as soil particle distributions (PSD), soil organic matter (SOM), total nitrogen (TN), total phosphorus (TP), cation exchange capacity (CEC), and exchangeable cations (K+, Na+, Ca2+, and Mg2+) were measured as potential explanatory factors of soil aggregate stability.[Results] 1) The stability of soil aggregates in different forest stands showed a trend of MWDFW < MWDST < MWDSW in general. 2) The soil aggregates stability of 4 forest stands showed a significant difference under different aggregate breakdown mechanisms. The soil aggregates of evergreen broad-leaved forest were the most stable while that of P. pubescens forest were very weak. 3) MWD of the surface soil was greater than that of the corresponding subsoil under the same stand, and the difference varied with different aggregate breakdown mechanism.4) Redundancy analysis (RDA) showed that the cumulative explanations of standard soil properties tested on soil aggregate stability were as high as 99.0%. The main factors influencing soil aggregate stability were different under different aggregate breakdown mechanisms. For FW and SW, soil aggregate stability was mainly affected by SOM, CEC, and exchangeable Mg2+, Ca2+. For ST it was mainly affected by exchangeable K+, Ca2+, Mg2+ and clay content. There was a significantly positive correlation between SOM and soil aggregate stability (P=0.004), and a negative correlation between exchangeable Na+ and the stability under three breakdown mechanism.[Conculsions] There are significant differences in soil aggregate stability in different stands, and the influencing factors are different under different aggregate breakdown mechanisms. Compared with the other three stands, evergreen broad-leaved forest demonstrate the most obvious effect on soil aggregates stability in this area. The mostly used average MWD of the 0-20 cm would, if the difference between surface soil aggregate (0-1 cm) and subsoil aggregate (>1-20 cm) is ignored, probably underestimate the aggregate stability of surface soil.
2020 Vol. 18 (2): 52-61 [Abstract] ( 430 ) [HTML 1KB] [PDF 918KB] ( 544 )
62 YANG Zhicheng, ZHANG Zhuodong, ZHANG Keli, WEI Xin
Spatial distribution of cropland soil erosion in Guizhou province based on sample data of the first national water census
[Background] The Karst region of Southwest China is characterized with the fragile ecological environment. Guizhou province is suffering from high intensity of soil erosion and sloping cropland is the most vulnerable to soil erosion in this region. Soil erosion of sloping cropland in Guizhou province had been studied on a provincial scale, and the results are beneficial to providing a basis for promoting soil and water conservation in this region. The spatial distribution and erosion intensity of cropland are greatly affected by regional divisions by geomorphy and topographic factors; therefore, it is necessary to take regional divisions and topographic factors into consideration to determine key areas for ecological restoration in this region.[Methods] 1) The digital map of regional divisions by geomorphy was created in ArcGIS 10.2 software according to related articles. 2) By using SPSS 19.0 software (Statistical Product and Service Solutions 19.0), we explored the proportion of cropland area and the cropland soil erosion intensity in Guizhou province. 3) By using ArcGIS 10.2 software, we built spatial distribution map of the proportion of cropland area and the cropland soil erosion intensity in Guizhou province.[Results] 1) The spatial distribution pattern of cropland area proportion in Guizhou province was obvious, which decreased from west to east. The proportion of cropland in non-karst plateau was the lowest, on the contrary, it was the highest in western Karst plateau. 2) The cropland with slope gradient of 8-35° accounted for 91.28% of the total cropland, and cropland with slope length >25 m accounted for 97.81%. With the increase of slope gradient, the soil erosion modulus increased correspondingly, especially in karst area; however, with the increase of slope length, the soil erosion modulus showed no obvious trend. 3) 71.17% of the total cropland area in Guizhou province belonged to middle erosion (<200 t/km2). The soil erosion in Peak-cluster depression and Karst fractured basin region were more serious with the acute erosion areas accounting for 34.97% and 15.16% of the total cropland, respectively.[Conculsions] On the whole, the Peak-cluster depression region and the Karst fractured basin region are the key areas for soil erosion control. These findings hold important implications for agricultural management, regional soil and water conservation and ecological management in Guizhou province.
2020 Vol. 18 (2): 62-68 [Abstract] ( 674 ) [HTML 1KB] [PDF 3054KB] ( 460 )
 
Applied Studies
69 LIU Jing, WANG Yong, HOU Ning, ZHANG Hanyu, ZHA Lin, LU Xiuyuan, LI Fucheng
Effects of wheat root on the characteristic of soil micro-aggregates at different slope positions of purple hill slope
[Background] The interaction between tillage erosion and water erosion causes soil and water losses in hilly croplands, which is a severe problem in hilly area with purple soil. In order to provide a scientific basis for the effects of wheat roots on water and soil conservation, the impacts of wheat roots on the composition and stability of soil micro-aggregates at different slope positions in purple soil were analyzed.[Methods] Two linear slopes were selected as the study site, which have an average gradient of 23%, and a horizontal length of 20 m. The whole slope was divided into 5 sample points:1 m, 5 m, 10 m, 15 m, and 20 m from the hill top to bottom. One slope where the typical wheat was cultivated was used as the treatment plot, while the other without wheat was used as the control plot. Five fractions (0.05-0.25 mm, 0.01-0.05 mm, 0.005-0.01 mm, 0.001-0.005 mm, and <0.001 mm) of soil micro-aggregates were obtained by field survey and laboratory analysis, and the micro-aggregates stability indicators included the mean weight diameter of aggregates (MWD), the mean weight soil surface area (MWSSA), and the fractal dimension (D).[Results] 1) The proportion of coarse fractions (0.01-0.25 mm) and <0.001 mm fractions in the treatment plot were higher than those in the control plot, especially at the 0 m slope position, while the 0.005-0.001 mm fraction was lower than that in the control plot. 2) In the range of 0-10 cm soil depth the significant differences (P<0.1) in MWD values were found at the 0 m, 5 m, and 20 m slope positions, with increments of 59.03%, 42.46%, 29.99%, respectively, and the MWSSA decreased compared with the control plot at the 5 m and 20 m slope positions. However, no significant changes were found at the other slope positions. The D was higher than that of the control plot except at the 5 m slope position. 3) The significant (P<0.1) increase of MWD by 38.23% was found at the 15 m slope position, while the MWSSA was lower than that of the control plot at 10 m, 15 m, and 20 m slope positions in 0-10 cm soil depth. 4) Correlation analysis indicated significant relationships between D and the proportion of <0.001 mm fraction (P<0.01).[Conculsions] Wheat roots in purple hillslope can intercept micro-aggregates of <0.001 mm and promote the polymerization from fine fractions (<0.01 mm) to coarse fractions (0.01-0.25 mm), and improve soil micro-aggregate composition. The root system of winter wheat presents the most significant effect on the stability of soil micro-aggregates at the boundary of the slope field (upslope and downslope positions).
2020 Vol. 18 (2): 69-76 [Abstract] ( 511 ) [HTML 1KB] [PDF 883KB] ( 460 )
77 ZHOU Mengling, GUO Jianbin, ZHOU Jinxing, WANG Lei, CHEN Xiao, YAN Weipeng
Characteristics of runoff and sediment yield from different vegetation types in the karst region of Danjiangkou Reservoir area
[Background] The purpose of this study is to quantify the response of runoff and sediment yield to the variation of rainfall and vegetation in the karst region of Danjiangkou Reservoir area, and to determine the optimal vegetation types for achieving the goals of soil erosion reduction and fragile environment restoration.[Methods] In 2018, a continuous monitoring was carried out for the runoff and sediment yield in standard runoff plots of 5 vegetation types (sparse forest of Vernicia fordii (Hemsl.) Airy Shaw (Ⅰ), forest of Pinus massoniana Lamb. (Ⅱ), slope farmland (Ⅲ), grassland (Ⅳ), shrubs of Sophora davidii (Franch.) Skeels (Ⅴ)). A correlation analysis was used to determine the main precipitation parameters which influence the runoff and sediment yield, and a t-test analysis was used to compare the impacts on the sediment yield among vegetation types.[Results] 1) The rainfall events with short duration and high intensity rainfall easily caused the runoff and soil erosion in this area, while the rainfall events with long duration and low intensity did not cause the runoff and soil erosion. 2) For all vegetation types, there was generally a significant (P<0.05), linear and positive correlation between the runoff and sediment yield and the rainfall parameters of rainfall depth and the maximum rainfall intensity (per 10 min, 30 min, and 60 min); while no significant (P>0.05) correlation existed for the rainfall duration and mean rainfall intensity. In addition, there was a significant linear and positive correlation between the sediment yield and runoff depth. 3) The reduction of total runoff by different vegetation types followed the order of:Ⅲ > Ⅱ > Ⅰ and Ⅴ>Ⅳ. The reduction of total sediment by different vegetation types followed the order of:Ⅱ > Ⅳ > Ⅰ and Ⅴ>Ⅲ. Except the insignificant (P>0.05) difference in the total runoff and sediment yield between the vegetation types of Ⅰ and Ⅴ, all differences between other vegetation types were significant (P<0.05).[Conculsions] The comparison of runoff and sediment yield among the vegetation types shows that the vegetation types of Ⅰ, Ⅲ and Ⅴ present a serious water and soil loss, and they require an urgent erosion control treatment. However, the vegetation type of Ⅱ presents a significant benefit of water and soil conservation. In order to intensify the control of rocky desertification and to increase the forest coverage in the study area, the benefits of soil and water conservation by forest/vegetation restoration sould be fully utilized. The results of this study offer a scientific basis for the ecological restoration aimed for the soil and water conservation in the karst sites of the Danjiangkou Reservoir area.
2020 Vol. 18 (2): 77-83 [Abstract] ( 581 ) [HTML 1KB] [PDF 2383KB] ( 476 )
84 ZHENG Miao
Litter and soil hydro-ecological effects of different stand types in the rocky mountain area of North China
[Background] The stony mountain area is the main forest distribution area in North China, and where is also an important water source area for Beijing and Tianjin City. To some extent, these forests in this area protect the ecological and water resources in North China. Therefore, there is great significance to study the hydro-ecological effects of different forest types in this area.[Methods] In order to explore the hydro-ecological effects of the litter and soil of the main forest types in this area, five typical stand types (Larix principis-rupprechtii forest, mixed forest of Pinus tabulaeformis and Quercus mongolica, Q. mongolica forest, mixed forest of Q. mongolica and Betula dahurica, and Lespedeza bicolor shrub) were selected as the research objects, and the indoor immersion method and ring knife method were used to measure the hydrological effects of litter and soil layer respectively.[Results] 1) The thicknesses of the litter under different stand types ranged from 21.3 mm to 37.1 mm, and the storage of litter ranged from 15.14 to 32.45 t/hm2. The capacity of maximum interception of litter ranged from 23.98 to 84.07 t/hm2. Among them, mixed forest of Q. mongolica and B. dahurica had the largest capacity of maximum interception and L. bicolor shrub had the smallest one. The capacity of the modified interception of litter ranged from 18.63 to 68.03 t/hm2, decreased by order of mixed forest of Q. mongolica and B. dahurica > Q. mongolica forest > mixed forest of P. tabulaeformis and Q. mongolica > L. principis-rupprechtii forest > L. bicolor shrub. On the whole, the capacity of the modified interception of litter of broad-leaved forest was generally higher than that of coniferous forest, and that of arbor forest was higher than that of shrub forest. 2) There was a logarithmic function relationship between litter water-holding capacity and soaking time (R>0.96), and a power function relationship between litter water holding rate and soaking time (R>0.98). 3) The soil density ranged from 1.06 g/cm3 to 1.19 g/cm3, and the soil saturated water-holding capacity ranged from 374.20 to 588.13 t/hm2, and the effective water-holding capacity ranged from 40.40 to 82.83 t/hm2, decreased by order of mixed forest of Q. mongolica and B. dahurica > Q. mongolica forest > mixed forest of P. tabulaeformis and Q. Mongolica > L. principis-rupprechtii forest > L. bicolor shrub. There was a power function relationship between the infiltration rate and infiltration rate of soil (R>0.99).[Conculsions] In summary, the water conservation functions of litter and soil layers are both the strongest in the mixed forest of Q. mongolica and B. dahurica. The management measures in the pure coniferous forest we suggested is that removing the coniferous tree and planting broadleaf tree to increase the water conservation capacity in the study area. Moreover, people should also strengthen the protection of broad-leaved mixed forests and broad-leaved forest and reduce the human disturbance to the shrub forest for improving the water conservation function in this area.
2020 Vol. 18 (2): 84-91 [Abstract] ( 561 ) [HTML 1KB] [PDF 888KB] ( 498 )
92 XIE Jinliang, ZHANG Jianfeng, LIU Yongbing, JIANG Jiuning
Heavy metal pollution and environmental assessment in the soil of the rare earth associated mining area in Bayan Obo
[Background] In view of the problems of over standard heavy metal content, serious environmental pollution and ecological damage in metal mining areas, the environmental assessment research on heavy metal contaminated soil was carried out. Bayan Obo mining area was dry and rainless, and the ecological environment was very fragile, coupled with the serious problem of desertification, thus environmental protection is needed.[Methods] Taking the soil of Baiyun Obo rare earth associated mining area as the research object, the soil contents of heavy metals, Pb, Cu, Zn, Cr, Ni and As, were analyzed by collecting 11 samples of 0-20 cm topsoil in different types of mining areas, i.e. main mine, east mine, dump, tailings pond, industrial site and transportation road. GB 15618-2018 The Soil Environmental Quality Risk Control Standard for Soil Contamination of Agricultural Land (Trial Implementation) and soil background values were used as evaluation criteria. The single factor method, Nemerow comprehensive pollution index method and pollution load index method were used to evaluate the contents of these six kinds of heavy metals. Soil environmental quality was evaluated in mining area. Using IDW interpolation analysis of ArcGIS 10.2 software, the spatial distribution characteristics of comprehensive pollution index value and pollution load index value were drawn, and heavy metal pollution evaluation was carried out.[Results] 1) The average values of Pb, Cu, Zn, Ni and As in the soil of the mining area exceeded 5.54, 2.37, 5.28, 1.69 and 1.10 times of the standard respectively, and the average values of Cr did not exceed the standard. The long-term human activitiy in the mining area was the major reason causing heavy metal pollution in the studied area soil. Pb, Cu, Zn, Ni and As were the main pollution elements, and their average contents were 942.42, 237.10, 1 585.43, 321.84 and 27.62 mg/kg, respectively. 2) From the perspective of sampling type, the contents of Pb and Zn in the studied soil were relatively high, and the pollution was the most serious. The order of Pb content was:East Mine > tailings pond > main mine > industrial site > dump > transportation road, and the order of Zn content was:Main Mine > tailings pond > dump > east Mine > industrial site > transportation road. Pb and Zn pollution was the most serious in the main mine and tailings pond, while Zn and Cu pollution was the main pollution in the dump. In addition, Ni pollution in the tailings pond and the dump was also serious. 3) The results by the 3 evaluation methods were basically similar. The pollution load index method based on the background value of the soil in the study area showed that the soil was polluted to varying degrees, the average PLI of the pollution load index was 2.58, which belonged to severe pollution.[Conculsions] Pb, Cu, Zn, Ni and As were the main pollution elements in the soil of the mining area. Pb, Zn and Cu in all sampling points exceeded the standard seriously, with the average exceeding rate of 90.91%, 100% and 100% respectively. Three evaluation methods showed that the main pollution in the mining area was Pb and Zn, followed by Cu and Ni pollution, no Cr pollution.
2020 Vol. 18 (2): 92-101 [Abstract] ( 487 ) [HTML 1KB] [PDF 2732KB] ( 536 )
102 ZHENG Xueliang, CHEN Lihua, LI Hongyang, TU Zhihua, GONG Wenyan, ZHANG Xueqi
Health assessment of Liaodong shelterbelt system based on water conservation
[Background] As a key component of terrestrial ecosystems, forest is of important ecological and social functions, while forest health is the prerequisite of ensuring the playing of these functions. Scientific assessment of the health status of forest stands can provide an important basis for function-oriented protection forest management.[Methods] Based on the survey data of forests health and the actual situation of shelterbelts in Dahuofang Reservoir, this study identified 4 aspects of "system vitality-organization-resilience-water conservation" as the criteria layer framework for the health assessment of water conservation forests, and then 17 indicators were selected to form a forest health assessment index system. The forest comprehensive health index (H) of different forest stands were calculated by the comprehensive index method, and according to 5 level of high quality, healthy, sub-healthy, unhealthy and disease, and the forest health for 5 typical shelterbelts (Larix gmelinii, Pinus tabuliformis, Pinus koraiensis, Robinia pseudoacacia and natural secondary forest) were analyzed.[Results] 1) The average forest heath comprehensive index of water conservation forest in Dahuofang Reservoir is 5.77, which is sub-healthy. Fifteen plots are in three states of healthy, sub-healthy and unhealthy, respectively, with the values of 7, 5 and 3 respectively. 2) For different forests, the forest health comprehensive index(H) of different forests ranks as natural secondary forest(7.29) > R. pseudoacacia(6.67) > P. koraiensis(5.88) > P. tabuliformis(5.79) > L. gmelin(3.21). Among them, the health status of the natural secondary forest is the best, and their forest structure, forest litter, and soil properties of forest land are obviously superior, with high structural stability and water conservation capacity. R. pseudoacacia is also in a healthy level, especially in terms of system vitality and water conservation. P. tabuliformis and P. koraiensis are in a sub-health state, and they have the conditions of transferring to healthy forests; L. gmelinii is unhealthy, which is significantly worse than other forests and needs to be improved.[Conculsions] The forests health of artificial forest is worse than that of natural secondary forest as its incomplete structure, the weak function stability, the weak anti-interference ability and the restoring force, and the weak ability of water conservation; the same is true for overall health values. Therefore, practical forest management measures should be taken to improve the health status of artificial forest, and natural secondary forests are a transformation target.
2020 Vol. 18 (2): 102-110 [Abstract] ( 529 ) [HTML 1KB] [PDF 830KB] ( 479 )
111 HU Yanting, ZHANG Fu, JIN Feng, WANG Shoujun, CAO Zhe, CHEN Tianlin, MOU Ji
On evaluation model of goal responsibility of soil and water conservation based on objectives and problems
[Background] Currently, there are differences in the types, intensities and hazards of soil erosion, the diversities and complexities of prevention and control tasks of soil erosion, and the imbalance of social and economic development in different administrative regions. It is difficult to measure the implementation of soil and water conservation work of local governments with a single soil and water conservation target responsibility indicator. Gansu province is one of the provinces with the most serious soil erosion. Therefore, establishing a soil and water conservation target responsibility assessment index system and assessment model composed of certain hierarchical indicators would help to accurately evaluate the level, science and integrity of soil and water conservation in Gansu province in terms of ecological environment construction.[Methods] The analytic hierarchy process(AHP) was used to construct the judgment matrix, calculate the index evaluation weight (W), and the test index rationality (indicator consistency ratio CR<0.1). After the index test was passed, the entropy method was used to modify the weight of the index evaluation obtained by the AHP, and determine the revised comprehensive evaluation weight (P), as well as to establish the assessment index system and evaluation model of Gansu province.[Results] Gansu province's soil and water conservation target responsibility assessment index system is constructed from the aspects of prevention and protection of soil erosion, comprehensive management, comprehensive supervision and accountability, the hierarchical structure consists of a target level (A), a criterion level (Bi), an operation level (Cj), and a sub-operation level (Dk). When establishing a water and soil conservation target responsibility assessment index evaluation model, the responsibility investigation is a negative impact indicator (2), and it is no need to give weights. The first-level indices are composed of three task indices, which are prevention and protection, comprehensive management and comprehensive supervision, whose comprehensive index evaluation weight is 0.400 0, 0.200 0, and 0.400 0, respectively. The rate of soil and water conservation schemes for production and construction projects is the largest (0.198 7) in the prevention and protection indicators of soil erosion, newly area of controlling water loss and soil erosion was the largest (0.120 0) in the comprehensive management indicators of soil erosion, supervision and law enforcement for development and construction projects is the largest (0.148 6) in the comprehensive supervision indicators of soil erosion. It focuses on the important indicators and direct indicators of the government's responsibility for soil erosion prevention and control.[Conculsions] The model consists of 3 first-level indices, 9 second-level indices and 17 third-level indices in Gansu province. There are 4 indicators of >10%:the rate of soil and water conservation schemes for production and construction projects (C3), protected area of key prevention region of soil erosion and water loss (C1), supervision and law enforcement for development and construction projects (D9) and newly area of controlling water loss and soil erosion (C4), accounting for 61.80% of the total weight. It fully reflects the requirements of prevention first, protection priority, emphasis and scientific management, which may provide a reference for the assessment of the target responsibility of soil and water conservation in Gansu province and similar areas, and offer the basic data for the implementation examination of national soil and water conservation planning.
2020 Vol. 18 (2): 111-119 [Abstract] ( 592 ) [HTML 1KB] [PDF 879KB] ( 422 )
120 WANG Minghao, WANG Xiuru, SUN Yan
Nitrogen absorption, distribution and utilization efficiency of summer maize plants under different biomass covering
[Background] The utilization efficiency of nitrogen fertilizer indicates the ability of crops to absorb nitrogen from soil and fertilizer. At the same time, nitrogen absorption and accumulation are the basis of crop yield formation. It is helpful to find out the relationship between the increase of crop yield and the efficient use of nutrients by investigating the accumulation of nitrogen uptake by crops. With a view to investigating the destination of nitrogen fertilizer and its use efficiency in plants under different farming modes, this paper explores the nitrogen use efficiency of plans employing the 15N isotopic tracer technique.[Methods] Three mulching modes, namely, biochar regulation (M1), combined regulation of biochar and straw (M2) and straw regulation (M3) were set up in the course of experiment, each containing three gradients, namely, 6 t/hm2 (F1), 12 t/hm2 (F2) and 18 t/hm2 (F3). The adsorption, distribution and use effect of nitrogen fertilizer in summer maize under different mulching control measures were investigated by analyzing the content change of marked nitrogen fertilizer in soil, the accumulation of nitrogen in plants and the source of nitrogen in each organ according to the field experiment.[Results] 1) The heat-retaining and water-holding capacity of straw and the physical and chemical properties of biochar significantly increased the content of inorganic nitrogen in soil. At the shooting stage, the average content of inorganic nitrogen in 0-80 cm soil layer under the M2F1 treatment condition was 11.71 and 20.25 mg/kg and higher than that under the M1FI and M3F1 conditions respectively. At the maturation stage, this average value under the M2F1 treatment condition was also remarkably higher than that under the M1F1 and M3F1 conditions. 2) Soil mulching regulation was effective in enhancing the accumulation effect of nitrogen in plants. The increase of mulching was accompanied by the marked rise of nitrogen content coming from nitrogen fertilizer. As shown by the analysis of the adsorption of labeled nitrogen by each organ, the results of 15N use efficiency in organs were as follows:Grain > Stem +leaf sheath > Root > Blade > Loquat + cob. The combined regulation of straw and biochar guaranteed the strongest nitrogen adsorption effect. 3) The results from Pearson and related analysis demonstrated that the biochar regulation effectively promoted the adsorption of labeled nitrogen fertilizer by root system, the combined regulation of biochar and straw facilitated the regulating effect of grain on marked nitrogen fertilizer and straw boosted the accumulation of marked nitrogen fertilizer in stalk + sheath.[Conclusions] The research may provide theoretical reference and technical support for the reasonable and effective development of agricultural water and soil resources and scientific guidance on agricultural fertilizer usage.
2020 Vol. 18 (2): 120-129 [Abstract] ( 549 ) [HTML 1KB] [PDF 1219KB] ( 422 )
 
Development Studies
130 WANG Meiqi, YANG Jianying, SUN Yongkang, WANG Gaoping, XIE Yuhong
Remote sensing rapid extraction technology for abandoned mine vegetation coverage via UAV
[Background] The excessive exploitation of mineral resources has caused the ecological environment of the mining area and its surrounding areas deteriorated severely, which has adversely affected human production and life. Vegetation restoration and reconstruction is an integral part of the ecological restoration work in mining area. Vegetation coverage monitoring is critical for mine greening restoration.[Methods] This study relied on field surveys and low-altitude aerial surveys of drones conducted in July 2018 to monitor the ecological rehabilitation benefits of an abandoned coal mine, Xiyuan Fourth Team Coal Mine Treatment Area in Fangshan district around Beijing, which underwent ecological restoration and control in 2016. In this study, a set of aerial image system for unmanned aerial vehicles (UAV) in the abandoned mining area with integrated stable gimbal and image acquisition was built based on a small multi-rotor drone and a ground control station. The drone flying height was 120 m, and the ground resolution of aerial images was 0.012 m. An accurate and fast method for extracting the vegetation coverage of the abandoned mine was proposed by converting drone images from RGB color space to HSV color space and limiting the range of H and S values. At the same time, the vegetation coverage of the same drone aerial image was extracted using the ENVI software via the supervised classification method to evaluate the extraction accuracy.[Results] The drone aerial photography was used to achieve the acquisition of high-resolution drone aerial images of centimeter-level vegetation in the abandoned mining areas, low system cost, simple maintenance and high efficiency. By converting the visible spectrum drone aerial image from the RGB color space mode to the HSV color space, the segmenting threshold value by limiting the S ≥ 0.2 and the H ≥ 47.1 allowed to quickly extract the vegetation part and further calculate the vegetation coverage to achieve accurate extraction with an error ≤ 6.857 6%, and under the same aerial photography conditions, the threshold settings of the S and H values were stable. Compared with the vegetation coverage extracted by supervised classification, the extraction result based on the HSV color space threshold segmentation method was lower, and the extraction error was getting smaller and smaller with the increase of vegetation coverage.[Conculsions] This study proposes a new method of quickly extracting vegetation coverage using drone aerial images, which provides a new idea for evaluating the ecological restoration effect of abandoned mines with high accuracy and efficiency.
2020 Vol. 18 (2): 130-139 [Abstract] ( 497 ) [HTML 1KB] [PDF 6263KB] ( 748 )
 
Forum
140 JIANG Dewen
Objectives and evaluating indicators of soil erosion control in the new era
[Background] China's economic and social development has entered a new era. It is of great significance to study soil erosion control targets and evaluation indicators to comprehensively control soil erosion and its impact, thus meeting the new needs of people in the new era for a beautiful ecological environment, and promoting the construction of a beautiful China.[Methods] This paper analyzed the characteristics of China's natural geography, the progress and effectiveness of soil erosion control, and the needs of economic and social development. It compared and analyzed the uncorresponding relationship between the area of soil erosion control and the area of soil erosion reduction and objective laws, and finally pointed out the ceiling constraints to soil erosion control.[Results] 1) The soil erosion will exist in China for a long time is the basic national situation. The sole goal of reducing the area of soil erosion is incomplete, in which there are shortcomings. 2) Reducing soil erosion intensity and its damage and restoring soil and water conservation functions should be the goal of soil erosion control in the future. Under the current economic and technological conditions, the soil erosion intensity, which we may achieve, is socially acceptable, and does not cause a major soil erosion hazard, should be applied as the approvable standards of control. Reducing soil erosion intensity should be the control standard for governance. 3) Based on the status of regional soil erosion, natural environmental conditions, economic development level, social needs, etc., the varied soil erosion control standards corresponding to types of national soil and water conservation divisions should be determined. 4) Different weights should be given to different effects of reducing soil erosion intensity. Monitoring and evaluation indicators of their own characteristics should be established in different leading functions area of soil and water conservation. 5) Reducing the soil erosion intensity, restoring and increasing the soil and water conservation function should be used as the evaluation basis and standard for determining the soil and water conservation rate in different regions.[Conculsions] The goal, standards, monitoring and evaluation indicators of soil erosion control in the era will be accordingly adjusted.
2020 Vol. 18 (2): 140-144 [Abstract] ( 668 ) [HTML 1KB] [PDF 699KB] ( 711 )
 
Research Review
145 SUN Liying, LI Qingya, CAI Qiangguo, CHEN Lajiao, WU Hui
Recent progress on ecosystem services functions of soil and water conservation measures
[Background] Soil and water conservation measures are critical for soil erosion control and land resources protection. Meanwhile, soil and water conservation measures provide various ecosystem services functions, such as regulation of hydrological flows, soil conservation and improvement, air purification, and wind and sand consolidation. In recent years, the ecosystem services functions of soil and water conservation measures have attracted considerable attention and become a hot spot, and understanding the ecosystem services functions of soil and water conservation measures would help to achieve harmony between human and nature.[Methods] Based on the available literature, we summarized the research progress on the ecosystem services functions of soil and water conservation measures. First we analyzed the concept and connotation on the ecosystem service functions of soil and water conservation measures. Then we classified the major ecosystem service functions of soil and water conservation measures. Further we summarized the evaluation systems for ecosystem services of soil and water conservation measures and classified the evaluation methodology adopted current research. Finally, we discussed the limits on the studies of ecosystem service functions of soil and water conservation measures, and highlighted research key points for future study.[Results] 1) Ecosystem services functions of soil and water conservation measures refer to the benefits derived from soil and water conservation, which help to protect and sustain human and natural environment, including regulating services, supporting services, provisioning services, and cultural services. 2) Quite a few studies have focused on basic theory of evaluation systems on ecosystem service functions of soil and water conservation measures, and few researchers established the evaluation index system. Current evaluation methods include:statistic data-based, and remote sensing, GIS and erosion models-based. 3) Issues of existing researches and the key points of future work are stated as follow. Firstly, the basic theory of evaluation systems on ecosystem service functions of soil and water conservation measures is weak, and thorough and authoritative index evaluation system is lack. Regional differentiation of soil and water loss should be taken into account in studying basic theory of evaluation systems on ecosystem service functions of soil and water conservation measures. Secondly, evaluation methods based on statistic data is restricted to assess the current or past ecosystem services functions of soil and water conservation; while methods based on RS, GIS and models mainly relied on empirical models and is lacking the ability in well represent the soil erosion process. More attentions should be paid to quantitative evaluation method for the higher accurate evaluation and prediction on ecosystem service functions of soil and water conservation measures. Thirdly, as spatial allocation of water and soil conservation measures determine landscape layout and ecosystem processes, the impact of spatial allocation of water and soil conservation measures on ecosystem service should be concerned in the future.[Conculsions] The research progress and future reseach points on the ecosystem service function of soil and water conservation measures are summaried, aiming atproviding readers guidelines for research, application and decision-making of soil and water conservation measures.
2020 Vol. 18 (2): 145-150 [Abstract] ( 618 ) [HTML 1KB] [PDF 810KB] ( 644 )
 
Academic Figures
151 LI Fei
LING Daoyang and China's soil and water conservation
[Background] The work of soil and water conservation in China has a long history, but the scientific research and subject development of Chinese soil and water conservation based on modern science has not been carried out until modern times. To study and sort out the literature materials of soil and water conservation in different historical periods plays an significant role in the research of the history of soil and water conservation development in the modern times of China.[Methods] This paper refers to the relevant archival materials collected by the Second Historical Archives of China, sorts of the modern times periodicals and magazines included in the Index of National Newspapers which were published by Shanghai Library, and also collects and arranges the relevant historical facts of LING Daoyang. Based on these original historical documents, the authors analyze and study the relationship between LING Daoyang and the development of soil and water conservation in modern times of China.[Results] Through the study, it is found that LING Daoyang is an early scholar who paid attention to soil and water conservation in modern times of China. In the theoretical aspect, he held that in order to revitalize the agricultural development, it was necessary to prevent soil erosion, and then LING Daoyang discussed the soil erosion situation at that time and its influencing factors. He concerned about the suffering of the people's livelihood and believed that preventing soil erosion can reduce the flood disasters occurred. With the deeper understanding of the soil erosion problems, he gradually formed the thought of comprehensive management of soil and water conservation with forestry measures as the core. In the practical aspect, he was involved in leading the work of soil and water conservation in the northwest area of China, and participated in surveying the work of soil and water conservation in the northwest area of China. Combining with the management work of the Yellow River Conservancy Commission, he promoted the project design and experimental construction of soil and water conservation. LING Daoyang led the establishment of the China Soil and Water Conservation Association and served as the first chairman of the China Soil and Water Conservation Association, which facilitated the scientific research and propagated the work of soil and water conservation in modern times of China.[Conclusions] Based on the analysis and research above the conclusion, we clearly realize that LING Daoyang is one of the most important pioneers of soil and water conservation in modern times of China, and he greatly contributed to the scientific research and practice of soil and water conservation in the modern times of China.
2020 Vol. 18 (2): 151-156 [Abstract] ( 438 ) [HTML 1KB] [PDF 996KB] ( 606 )
中国水土保持科学
 
Notice on the Recruitment of Youth Editorial Board Members for the Journal of SSWC
Theme on Spreading Spirits of Great Scientists: LIANG Xi, the Founder of Forestry Education in China
ZHENG Fenli, CHEN Liding and LEI Tingwu in the list of Highly Cited Chinese Researchers by Elsevier
SSWC Indexed in the 2020 edition of “A Guide to the Core Journals of China”
Science of Soil and Water Conservation Accepted for Inclusion in Scopus
2020 Editor-in-Chief Meeting of Science of Soil and Water Conservation Held in Beijing, Concurrently
SSWC Selected to Be in Core Library of Source Journals of CSCD during 2019-2020
SSWC Indexed in the 2017 edition of “A Guide to the Core Journals of China”
Appreciation for peer reviewer of SSWC Editorial Board
2017 Editor-in-Chief Meeting of Science of Soil and Water Conservation Held in the Yangling of Shaan
Professor Wang Lixian, Former Editor-in-Chief of SSWC Won Norman Hudson Memory Award
Calls for Papers in English
Deputy Editor-in-Chief Cui Peng Elected as a Member of 9th National Committee of CAST
Three Members of SSWC Editorial Board Rewarded as NOSTW in 7th Session Assessment
Election of 4th Editorial Board and First Meeting of New Board Held in Beijing
Deputy Editor-in-Chief of SSWC, Academician Cui Peng elected as a member of the IRDR SC
Notice About The 5 Not-Allowed Rules While Publishing Academic Articles by 7 Organizations
SSWC Indexed in “A Guide to the Core Journals of China”
Science of Soil and Water Conservation Calls for Papers
SSWC Selected to Be in Core Library of Source Journals of Chinese Science Citation Database During
On the Home Page of the Journal Science of Soil and Water Conservation
Five Papers of Science of Soil and Water Conservation Determined as Excellent in 5th Assessment
Congratulations to Deputy Editor-in-Chief Cui Peng Elected as Academician of Chinese Academy of Scie
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