中国水土保持科学
中国水土保持科学
 
 
 
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2020 Vol.18 No.6  Published 2020-12-30
  
 
Yellow River Basin
1 YANG Meng, SONG Xiaopeng, ZHANG Yan, DENG Jiayong, ZHAO Yiyang
Distribution of sloping cropland and correlative erosional landform in typical watersheds on the hilly Loess Plateau
[Background] Sloping cropland is subject to most serious soil erosion in the Loess Plateau. Although the conversion of cropland to forests or grassland has been implemented for nearly 20 years, cropland on steep slope still exists in the hilly Loess Plateau which is in need of detailed survey and effective management. [Methods] Chabagou and Qingshuigou in Zizhou county, Shaanxi province which are also in the flooding area of "7·26" torrential rainstorm were selected as typical watershed of the type I area of the hilly and gully region of the Loess Plateau to compare distribution of sloping cropland between watersheds with and without comprehensive management. Based on high-resolution satellite remote sensing and UAV images, GIS technology was used to extract and analyze sloping cropland area and its distribution. Topographic map with a scale of 1:10 000 and Digital Surface Models (DSM) were used to extract and analyze topographic parameters such as slope gradient, slope length, slope position and upslope catchment area. [Results] 1) In 2017, the area of sloping cropland accounted for 11.08% of the total area of Chabagou watershed. Sloping cropland area in Shejiagou, a branch watershed of Chabagou with comprehensive management, accounted for 6.90%, and that in Qingshuigou watershed, with serious soil erosion causing the dam break during "7·26" rainstorm, accounted for 11.15%. 2) The average gradient of the sloping cropland in Qingshuigou was 32.54°, of which the ratio >25° accounted for 94.01%. The average gradient of the sloping cropland in Shejiagou was 20.62°, of which the ratio > 25° accounted for 36.47% and the ratio > 15° accounted for 79.62%. The average slope length of sloping cropland in Qingshuigou and Shejiagou was 38.50 m and 32.58 m respectively, of which 94.06% and 86.12% was over 20 m. More than 70% of sloping cropland in Qingshuigou and less than 50% in Shejiagou belonged to the long-steep sloping cropland. 3) More than 99% of the sloping cropland of Shejiagou and Qingshuigou catchment areas were located in the middle slope position and only a few were located in the upper slope position. Compared with in Qingshuigou, the ratio of upslope catchment area to sloping cropland area in Shejiagou was larger. [Conculsions] There is still a certain proportion of steep sloping cropland in the type I area of the hilly and gully region of the Loess Plateau which is an important source of runoff and sediment. The lack of attention to the statistics of steep sloping cropland has greatly increased the risk of severe soil erosion and flood disasters under extreme precipitation conditions.
2020 Vol. 18 (6): 1-8 [Abstract] ( 440 ) [HTML 1KB] [PDF 6445KB] ( 600 )
9 QIAO Rongrong, JI Shuxin, BAI Xuelian, WANG Lixiang, CHANG Xueli
Relationship between gully quantitative characteristics and soil erosion amount
[Background] Soil erosion is one of the serious phenomenon during the soil degradation process, and it directly affects the ecological environment and local economic development. The quantitative characteristics of the gully, which is a principal component factor for assessing the soil erosion intensity, plays an important role in saving water and soil conservation study. [Methods] Based on the DEM data at 30 m resolution, this paper used the Universal Soil Loss Equation (USLE) and the ArcGIS Hydrological Analysis Module to analyze the gully quantitative characteristics and soil erosion status of the typical secondary tributary watershed in the Yellow River Basin. According to the yearly soil erosion modulus, four grades were divided by using the occurred frequency of the annual modulus. Then, typical years were selected by using closest to the average soil erosion modulus on each grade. Finally, the relationship between soil erosion amount and gully quantity characteristics (gully length, basin area, and gully density) at the different grades was analyzed. [Results] The gully length was distributed in 0.26-154.41 km with an average of 9.41 km while the basin area was distributed in 0.73-177.03 km2 with an average of 10.57 km2. Gully density was distributed in 0.36-2.34 km/km2 with an average of 0.94 km/km2. The variation of soil erosion modulus during the study period (2000-2017) was from 11.84 to 72.83 t/(hm2·a), and showed a fluctuation increasing trend. Frequency analysis indicated there were four grades as 0-20, 20-30, 30-50 and 50-80 t/(hm2·a), and best match years were 2015, 2006, 2004 and 2016, respectively. In these typical years, soil erosion amount increased significantly with the increase of gully length and basin area, and the gully length of any typical year has a faster regression response rate than the basin area. Soil erosion amount changed irregularly with the increase of gully density. [Conclusions] The gully length and basin area were mainly concentrated in < 10 km and < 10 km2, which accounted for 80.11% and 78.45% of the total, respectively. The density of gully was mainly concentrated between 0.5-1.5 km/km2, which accounted for 92.82% of the total. There was a significant linear regression relationship between the soil erosion amount and the gully length and basin area (Sig.<0.001). The erosion modulus of different grades had the same pattern. Therefore, the soil erosion amount of the corresponding watershed can be obtained more simply and directly by gully length or basin area. On the whole, there was no significant linear regression relationship between gully density and soil erosion amount, but there was a higher amount of soil erosion than the overall level when the gully density between 0.74-0.98 km/km2, and its mean value was 6 times as much as the others.
2020 Vol. 18 (6): 9-14 [Abstract] ( 395 ) [HTML 1KB] [PDF 1337KB] ( 476 )
15 CHAI Yuanyuan, XIONG Lifeng, LUO Jinxuan, ZHANG Runxia
Division and calculations of the artificial ecological water demand types in the New District of Lanzhou city
[Background] The research of ecological water demand is very beneficial for the ecological irrigation practice and sustainable development and utilization of water resources in this region. [Methods] In this paper, the New District of Lanzhou city was taken as the study area, and the current artificial ecosystem of this region was divided into three categories that consisted of 13 sub-items in total through consideration of the similarities of ecosystem functioning and water demand characteristics by employing the ArcGIS 10.2 software technology. The water demand of these three categories in 2016, 2020, 2030, which included the vegetation, the artificial water body and the ecological type of urban construction, were calculated by utilizing different methodologies, respectively, such as the combination of the Penman-Monteith method and crop coefficients, the recharge and evaporation of water surface, water quota per unit area. The implementations of these calculations are on the basis of several data sources such as remote sensing image, meteorological data and the regional ecological planning, et al. [Results] 1) The total area of ecological water demand in 2016 was 39.55 km2, among of which, the ecological water demand of vegetation, artificial water body and urban construction were 24.57 km2, 5.22 km2 and 9.76 km2 respectively, the water demand quota were 675.5 mm, 820.3 mm, 731.0 mm, respectively. 2) The total ecological water demand in the study area in 2016 was 28.01×106 m3, including 16.6×106 m3 for vegetation, 4.28×106 m3 for artificial water body and 7.13×106 m3 for urban construction. 3) The total ecological water demand of the research area in 2020 was 55.79×106 m3, including 33.30×106 m3 for vegetation construction, 6.06×106 m3 for artificial water body and 16.43×106 m3 for urban construction. 4) The total ecological water demand of the research area in 2030 was 58.44×106 m3, including 35.20×106 m3 for vegetation, 6.81×106 m3 for artificial water body and 16.43×106 m3 for urban construction. [Conculsions] The ecological area and water demand are gradually increasing, and the departments should provide sufficient water resources for the artificial ecosystem according to the characters and weights of the water utilization of different ecology types, which can be beneficial for the stable development of ecological system.
2020 Vol. 18 (6): 15-23 [Abstract] ( 515 ) [HTML 1KB] [PDF 3210KB] ( 436 )
24 ZHANG Xingxing, LIU Xiaofang, ZHAO Yonggang, DU Yujia, JIA Jiayu, REN Zeying
Spatial heterogeneity of soil moisture on slopes of Caragana korshinskii Kom. plantations and its main controlling factors in loess hilly region
[Background] The typical shrub species Caragana korshinskii Kom. is widely planted in the vegetation construction, and plays an important role in ecological restoration and soil erosion control in the arid and semi-arid area. [Methods] Four landscape transects including 15-, 25-, and 35-year-old C. korshinskii Kom. plantations with shrub belt and grass belt, and natural grassland (as control) were selected in the loess hilly region. Heterogeneity of soil moisture content at 0-100 cm depths and its main environmental impact factors were analyzed using redundant analysis. [Results] The soil moisture content on the slope of the study area ranged from 3.3% to 21.3%, showing a moderate variation. With increasing plantation years of C. korshinskii Kom., the values and variability of soil moisture content gradually decreased. The slope positions also had significant effects on soil moisture content, which showed an order of lower-slope > top-slope > mid-slope > upper-slope > shoulder-slope. With the increase of the plantation years of C. korshinskii Kom., the differences of soil moisture content between shrub belt and grass belt decreased, and showed positive values at all slope positions except for the top-slope position. Redundant analysis and variance partitioning analysis showed that plantation age and altitude were the main factors affecting soil moisture heterogeneity, followed by slope position, slope, coverage and belt. The explanation variances of soil moisture content by plantation age, altitude, and slope position were 1.9%, 6.1%, and 3.0%, respectively, and the integrated explanation variance by all environmental factors reached 74.4%. [Conclusions] Overall, the plantation of C. korshinskii Kom. in the loess hilly region reduced soil moisture content and its heterogeneity. Therefore, the synergy effects between the plantation ages of C. korshinskii Kom. and topographic factors should be considered for the distribution patterns of soil moisture content during regional vegetation restoration.
2020 Vol. 18 (6): 24-32 [Abstract] ( 407 ) [HTML 1KB] [PDF 3073KB] ( 380 )
 
Foundamental Studies
33 LIANG Shizhengxiong, FANG Haiyan
Dynamic changes of soil erosion in Qiantang River Catchment from 2006 to 2015
[Background] Understanding soil erosion is an important prerequisite to prevent land degradation, river siltation, and water pollution through implementing soil conservation measures. Large terrain fluctuation and strong rainfall intensity characterize the red soil region in southern China, where soil erosion is second only to the Chinese Loess Plateau. Acting as an economically developed area and an important fresh water area in Zhejiang province, the Qiantang River Catchment (QRC) suffers from severe soil loss. However, soil erosion characteristics, influencing factors, sediment sources, and their changes during the recent past years are seldom investigated. It is urgently required to identify the changing trend and influencing factors of soil erosion in the QRC. [Methods] Based on digital elevation model (DEM), soil property, Normalized Difference Vegetation Index (NDVI) derived via Moderate-Resolution Imaging Spectrometer (MODIS), and rainfall datasets, the Revised Universal Soil Loss Equation (RUSLE) was used to simulate soil erosion during 2006—2015 in the QRC, and the spatio-temporal characteristics of soil erosion were analyzed. Then, the monitored sediment yield data was used to calibrate the estimated results. The soil erosion intensity index was further calculated to quantify the changing trends of soil erosion for different land use types. A regression model was also established to quantify the separate contributions of rainfall erosivity and land use to the changed rates of annual soil erosion [Results] 1) There were great spatial variations of soil erosion in the QRC. Because slight soil erosion (i.e., with soil erosion rate <500 t/(km2·a) dominated the study area, and higher erosion rates scattered the QRC, this kind of soil erosion was concealed and easily ignored. The soil erosion rate reached 1 605.82 t/(km2·a) in 2015 and was closely related to topographic factors and land use patterns. The total amount of soil loss reached 6 375.74×104 t in the QRC. Higher soil erosion rates occurred on the grass- and forest-lands, with slope gradients ranging from 15 to 35°. These lands were widely distributed in the QRC and should be the priority areas for future soil loss control. 2) In recent ten years, mainly affected by precipitation and vegetation cover, annual soil erosion rates in the QRC increased insignificantly. The contributions of annual rainfall erosivity and vegetation coverage to the increased soil erosion were 60% and 32%, respectively. Land use change in the study area benefited to soil loss control. However, it could not offset the impact of increased rainfall erosivity on soil erosion. 3) Soil erosion intensity index effectively reflected the impact of land use on soil erosion. Through assuming that rainfall erosivity remained constant in 2015, the soil erosion intensity indices in different land use types during 2006—2015 were calculated, and it was found that the unused- and grass-lands had high soil erosion intensity indices, which reached 248.6 and 214.37 respectively. Therefore, future implementation of soil conservation measures also should be strengthened on these lands. [Conclusions] The spatial variations of soil erosion and its annual changes during 2006—2015 were obtained by using RUSLE. Topographic factors and land use controlled its pattern of spatial variation, and rainfall erosivity and land use determined the annual changes of soil erosion. In the QTC, soil erosion mainly was from grass- and forest- lands on the steep slopes. In recent years, the unused land also experienced high soil erosion rate. More attentions should be paid to these types of lands in the future implementation of soil conservation measures.
2020 Vol. 18 (6): 33-42 [Abstract] ( 540 ) [HTML 1KB] [PDF 3345KB] ( 464 )
43 LIANG Chunlin, WANG Bin, ZHANG Wenlong
Stability and structural characteristics of soil aggregates on sloping farmland in black soil region, Northeast China
[Background] As an important grain production base in China, the black soil area of Northeast(NE) China suffers from serious soil erosion. Soil aggregate stability has profound impact on soil erosion processes. To compare the susceptibility of soil aggregates for surface/subsoil, different aggregate breakdown mechanisms should be considered. The objectives of this study were to assess the variations between surface soil and subsoil aggregate stability under different breakdown mechanisms, and to quantify changes of the micro-structural characteristics, provide theoretical basis for soil erosion control of slope farmland during rainy season. [Methods] Based on line-transect sampling, six typical slopes were selected as the research areas in the black soil region of NE China. Seventy-two top-surface (0-1 cm) and subsoil (1-10 cm) of undisturbed soil samples were collected from ridges and ditches on the typical slopes randomly. Soil aggregate stability was determined by Le Bissonnais (LB) method, including fast wetting (FW), slow wetting (SW) and stirring (ST) treatments, and structural characteristics were observed by scanning electron microscope (SEM). In addition, soil organic matter (SOM), cation exchange capacity (CEC), soil mechanical composition and pH were determined separately, to clarify the stability and structural differences of surface soil and subsoil aggregate. [Results] 1) The soil texture of each typical slope was loam, and the clay content was 15.6%-20%; CEC varied from 19.8 to 44.2 cmol/kg, and the surface soil was slightly higher than the subsoil. The average value of SOM in surface soil is 31.48 g/kg, which is lower than 40.78 g/kg in subsoil. The porosity of soil aggregates in the surface soil is slightly higher than that in the subsoil, but there is no significant difference. 2) Soil aggregates in FW treatment were mainly converted to <0.2 mm particle size, and the conversion ratio of surface soil was 62.6%-76.2%, and that of subsoil<50%;. After SW treatment, soil aggregate was mainly converted to>0.2 mm particle size, and the conversion ratio of subsoil was 1.11-5.69 times that of the surface soil. After ST treatment, the subsoil aggregate>5 mm particle size accounted for 65%, and the surface soil was 39.8%. 3) The SEM area porosity of soil aggregates varied from 7.43% to 23%, and the porosity of the surface soil aggregates was higher than that of the subsoil aggregates. Under FW treatment, soil aggregates with high porosity tended to be breakdown; the lower the SOM and CEC were, the higher the soil aggregate porosity was. Compared with subsoil aggregates, surface soil aggregates had more porosity and larger average area. [Conclusions] 1) The subsoil aggregate stability is significantly higher than that of the surface soil, and represents the order as MWDFW < MWDSW < MWDST. 2) There is a significant positive correlation between MWD and SOM of soil aggregates, and shows a significant negative correlation with soil porosity. MWDFW can be used as a key indicator for the stability of black soil aggregates. 3) The stability of soil aggregates in typical black soil area is mainly determined by pore size and quantity.
2020 Vol. 18 (6): 43-52 [Abstract] ( 561 ) [HTML 1KB] [PDF 2801KB] ( 438 )
53 LI Kunheng, Lü Gang, QIN Wei, MA Junhui, LI Yexin
Infiltration characteristics of urban soil in semi-arid area of western Liaoning province
[Background] In order to reveal the infiltration characteristics and influencing factors of typical urban soils in semi-arid areas of western Liaoning, taking Fuxin city located in the western Liaoning region as an example, the infiltration capacity of urban soil in Fuxin city and its influencing factors were studied, from the angle of the soil infiltration to discuss the reason of urban waterlogging in western Liaoning flood season. [Methods] The method of combining the field double ring infiltration with the indoor analysis was used to systematically analyze the physical and chemical properties and infiltration characteristics of eight different types of urban soils, Using Horton model, Kostiakov model and Philip model, the urban soil infiltration was fitted by Origin 9.1 software. [Results] The bulk density of urban soil in Fuxin is 1.23-1.44 g/cm3, and the bulk density of green land is the smallest. The overall soil shows the characteristics of low organic matter content, high sand content (all above 72%) and poor soil viscosity. Compared with the original soil in the suburb, the soil compactness and texture in urban area are significantly different. The stable infiltration rate of remolded soil of park green space is 2.04 mm/min, which is not significantly different from the stable infiltration rate of primary soil in suburb, which is 1.15-4.00 times of that of other types of urban soil. The stable infiltration rate of different types of urban soil is negatively related to bulk density, positively related to total porosity. The goodness of fitting regression models for different types of urban soil infiltration process is Horton model > Kostiakov model > Philip model,Horton model can be used as the best model to simulate and predict the urban soil infiltration process in Fuxin. In Fuxin city, the distribution of stable infiltration rate grades of urban soil is relatively concentrated, with slow and medium infiltration rate grades accounting for 12.5% and 75.0% respectively, and the infiltration capacity of urban soil is weak. [Conculsions] Human activities lead to compaction of urban soil to different degrees, change the soil structure, and weaken the infiltration capacity of urban soil. The soil infiltration classification in Fuxin city was mainly in the slow and medium grades, and the soil infiltration capacity is weak, which is one of the reasons for urban waterlogging in flood season. Increasing the area of urban green space and enhancing the management and maintenance of urban green space to improve the soil structure is the key to improving the function of urban soil water conservation.
2020 Vol. 18 (6): 53-61 [Abstract] ( 446 ) [HTML 1KB] [PDF 911KB] ( 450 )
62 ZHOU Zhuangzhuang, REN Zongping, LI Peng, XIE Mengyao, LI Zhanbin, XU Guoce
Response of soil moisture content to precipitation under different vegetation coverages
[Background] Soil moisture content is one of the key factors in the Loess Plateau for managing the vegetation ecosystem, and the response characteristics of soil moisture to precipitation under different vegetation cover have important theoretical significance for the sustainable development of regional vegetation. [Methods] The soil content were measured each hour by the multi-depth soil moisture instrument (ET100-5AH) in three slopes with vegetation coverages at 30%, 70% and 90% respectively in the 2017. And also, the hourly rainfall data was collected from the local weather station for studying the relationship between the soil content and rainfall. Then, the threshold affecting soil moisture content change was defined in different rainfall conditions. Based on those data, the rainfall events were classed 4 groups by the rainfall characters, such as rainfall volume, the rainfall duration, and so on. The difference of soil contents under the different vegetation conditions were analyzed, then the soil moisture response relationship of precipitation was furthered studied to define the thresholds that affected soil moisture changes under different rainfall conditions. The soil content changed corresponding to the storm heavy rainfall was specially studied. [Results] 1) The threshold for rainfall volume that affected the soil moisture content of the layer 10, 20, 40, 60 and 80 cm depths were more than 6.8, 12.6, 41.2, 43.8 and 83.0 mm respectively. 2) Under the process of continuous precipitation with low initial intensity, the soil moisture content of the medium cover grassland B was higher than that of the low cover grassland A, and that of high cover mix woodland C was the lowest,the response of soil moisture content of grassland within 1-4 h of precipitation appeared. 3) The response time of 0-100 cm depth soil moisture content of the mixed forest to storm rainfall was longer than of the low cover grassland A and the medium cover grassland B. 4) The minimum value of primary precipitation triggering the response of soil moisture content for the medium B and the low cover grassland A was the same (0.2 mm), while the response of the high cover mix woodland C required higher precipitation and soil moisture content (1.0 mm). [Conclusions] Long duration storm with higher peak intensity are conductive for the soil infiltration and soil moisture accumulation. Then this rainfall pattern is the main source of replenishment soil moisture content for this study area. The soil content of high-coverage is generally lower than that of low-coverage, and the soil infiltration volume has the similar trend with the soil moisture content. Considering the limited rainfall in this area and the soil moisture content, the grass planting may be more suitable for the protecting local water soil resources.
2020 Vol. 18 (6): 62-71 [Abstract] ( 442 ) [HTML 1KB] [PDF 3925KB] ( 406 )
72 DAI Songjia, ZHOU Chenni, DUAN Fei, FANG Jiangping, LONG Chunlin
Effects of composition and habitat differences on litter decomposition and nutrient release characteristics of Abies georgei var. smithii in southeastern Tibet
[Background] Litter decomposition is one of the important links of material cycle and energy flow in forest ecosystem. There are few reports on the litter decomposition and nutrient release of typical natural dark coniferous forests in Tibet. The purpose of this study is to provide basic data and theoretical basis for in-depth understanding of the material cycle process of forest ecosystem in high altitude and cold environment. [Methods] Three types of samples (leaf sample, natural sample, and branch sample) from 3 sample plots (in forest, outside forest and beside forest) were selected in Sejila Mountain, Tibet. The litter of Abies georgei var. smithii forest was collected in December 2016. At the beginning of each month in 2017, 3 bags of litters were collected from each sample plot, and the litter retention rate and monthly decomposition rate were calculated. The content of C, N, P, and K was determined by concentrated sulfuric acid-potassium dichromate method, Kjeldahl method, molybdenum blue colorimetric spectrophotometry, flame spectrophotometry. [Results] 1) The monthly decomposition rate of litter was leaf sample (2.21%) > natural sample (2.17%) > branch sample (1.70%), and IF (2.17%) > OF (1.94%) > BF (1.93%). 2) The decomposition time of 95% of natural sample, leaf sample and branch sample litter in the same habitat with different components was 8.96 years, 10.02 years and 13.18 years. 3) The decomposition time of 95% of IF, OF, and BF with the same component was 8.96 years, 10.01 years and 10.84 years. 4) The release rates of C and N were significantly positively correlated with the components, while the release rates of P and K were negatively correlated with the components. 5) The release rates of C, N, P and K were significantly or very significantly and positively correlated with the habitat. 6) There were significant differences in C/N, C/P and N/P among different habitats. 7) There was a very significant negative correlation between C/N and habitat, no significant correlation between C/P and habitat, and an extremely significant positive correlation between N/P and habitat. [Conclusions] Different litter components and habitat conditions have significant effects on litter decomposition rate and nutrient release characteristics, and the effects of components and habitats vary.
2020 Vol. 18 (6): 72-80 [Abstract] ( 386 ) [HTML 1KB] [PDF 1056KB] ( 520 )
81 ZHANG Xue, WANG Dongmei, WEN Wenjie, LIU Ruosha, LI Ping, ZHANG Peng
Ecological stoichiometric characteristics of plantation soil in the Tibetan Plateau-Loess Plateau transition zone
[Background] Due to the special geographical location, the ecological environment of Tibet Plateau-Loess Plateau transition zone is fragile and its soil fertility is quite poor. Plantation is the main measure of ecological restoration in this area. Studying the soil ecological stoichiometric characteristics of plantation is conducive to understanding the effect of vegetation improvement in this area and revealing the limiting elements of vegetation growth, providing theoretical basis and technical guidance for vegetation restoration and reconstruction. [Methods] The study selected 5 standard plots (20 m×20 m) for each plantation(Picaea crassifolia, Sabina przewalskii, Pinus tabuliformis Carr., Larix principis-rupperchii, Populus cathayana Rehd, and Betula platyphylla Suk) in this area, and selected 3 standard plots (20 m×20 m) of grassland as a control. We collected 0-60 cm soil samples to determine their C, N and P contents, using one way ANOVA and Pearson correlation analysis to explore the soil ecological stoichiometric characteristics of typical plantations and their influencing factors. [Results] 1) The soil C, N and P contents of 6 plots were 11.34-20.86, 1.16-1.74 and 0.51-0.72 g/kg. The soil nutrient contents of each plantation were higher than that of grassland, while the soil nutrient of broad-leaved forest was higher than that of coniferous forest. 2) The soil C/N, C/P and N/P of 6 plantations were 9.30-11.60, 16.56-41.98 and 1.71-3.64. The soil C/P and N/P were lower than the average level of soil in China. 3) Soil C, N and P decreased with the increase of soil depth, and there were significant differences between different soil layers (P<0.05). Soil C/N decreased with the deepening of the soil depth, and its coefficient of variation was small. Soil C/P and N/P of different plantations showed different trend of soil depth, while they had no significant difference between different soil layers. 4) The correlation analysis showed that there was a very significant positive correlation between soil C and N, indicating that the changes of their contents were consistent. C/P and N/P were more affected by P. Soil nutrients and their stoichiometric ratio were significantly correlated with soil saturated hydraulic conductivity and alkali-decomposed nitrogen (P<0.05). [Conclusions] This study indicates that plantation has a certain improvement effect on soil nutrients, while broad-leaved forests are better than coniferous forests. N is found to be the main restricted nutrient in this area. In the process of plantation management, attention should be paid to the supplement of N to promote the healthy development of plantation ecosystem.
2020 Vol. 18 (6): 81-89 [Abstract] ( 260 ) [HTML 1KB] [PDF 987KB] ( 476 )
90 XIN Zhiyuan, XIA Jianguo
Spatial distribution characteristics and reserve estimation of soil organic carbon in the hydro-fluctuation belt of the Pubugou reservoir
[Background] Previous studies demonstrate that the global CO2 emissions and climate warming is affected by reserves and distribution of soil organic carbon. Subsequently, the release of soil organic carbon is serious due to the frequent alternations of dry and wet in the hydro-fluctuation belt. The water level difference in the hydro-fluctuation belt of the Pubugou reservoir reaches 60 m, and the nutrient loss is serious because of the complex terrain combined with special dry and hot climate. However, no relevant research has been reported yet. [Methods] The 0-40 cm soil of the hydro-fluctuation belt in the Pubugou reservoir in southwestern China was selected to gain insight into the spatial distribution of soil organic carbon and its storage estimation. The survey and investigation of the site was conducted by the total station instrument, and the soil samples were collected separately based on the land use and land cover (LULC), altitude and terrain. The reserves of soil organic carbon of the hydro-fluctuation belt were estimated by using the collected samples, analyzing distribution characteristics of soil organic carbon, and excluding the interaction effect of three factors with the ArcGIS software and testing the data of soil sample. [Results] 1) In the hydro-fluctuation belt, the content of soil organic carbon decreased with the soil depth increasing, which changed with a value of 14.75, 12.19 and 9.70 g/kg in the soil layer of 0-10 cm, 10-20 cm and 20-40 cm, respectively. 2) The average value of soil organic carbon under different LULC was detected as follows: sludge>grassland>dryland>bare land. 3) The content of soil organic carbon was also inversely proportional to the LS value of terrain factor. 4) The total soil organic carbon reserves at 0-40 cm depth were 184 134.14 t, and the mean density was 6.29 kg/m2. After deducting the 2.21 hm2 area of dam and bare rock, the mean density was 6.80 kg/m2. In the soil layer of 0-40 cm, the high storage density of soil organic carbon was found in grassland and sludge. Additionally, the area of low storage density showed a substantial amount of bare land. [Conclusions] This research reveals the spatial distribution characteristics of soil organic carbon, meanwhile the estimation of soil organic carbon reserves in the hydro-fluctuation belt of the Pubugou reservoir are also illustrated. It proves a new method for multi-factor calculation of soil nutrient reserves and also provides basic scientific data for ecological protection in the research area.
2020 Vol. 18 (6): 90-98 [Abstract] ( 396 ) [HTML 1KB] [PDF 3023KB] ( 408 )
99 LI Zhiguang, WANG Yongsheng
Targets and tasks of China's soil erosion comprehensive supervision and its approaching way in the New Era
[Background] The essence of soil erosion supervision is to adjust human behavior and correct human improper behavior to control soil and water loss. The work focus of China water and soil conservation has tended to soil erosion supervision since 2018, and the ability of public service and social governance has been improved obviously, but the contradiction between insufficient of soil erosion supervision and social demand is prominent day by day. [Methods] Based on the experiences and lessons of soil erosion supervision and research on monitoring of soil and water conservation, according to the demand for soil and water conservation in social and economic development, government decision and public activities, this paper comprehensively analyzed the meaning and work flow of soil erosion supervision, and put forward the targets and tasks of soil erosion supervision and its realization way. [Results] The targets of soil erosion supervision include exploring and discovering soil erosion and its influencing factors, evaluation and prediction soil loss and the harmfulness, demonstration on prevention and management of soil and water loss, supervision and law enforcement to prevent artificial soil loss. The soil erosion supervision contains seven tasks, which could be implemented by spatial organization, time organization and organizational implementation, and improvement of national standards, popularization and application of modern space technology, construction and application of information system and construction of supervision team can provide important technical support for the soil erosion supervision. [Conclusions] This paper point out that soil erosion comprehensive supervision should be a closed-loop system which consists of data acquisition and analysis and its application to soil erosion comprehensive supervision, all the tasks and technical support measures should make concerted efforts in promoting soil erosion supervision system becoming more mature, and this research can provide a reference for governments at all levels in soil erosion comprehensive supervision.
2020 Vol. 18 (6): 99-104 [Abstract] ( 503 ) [HTML 1KB] [PDF 2396KB] ( 480 )
 
Applied Studies
105 XIE Yun, GAO Yan, GU Zhijia, LIU Gang, GAO Xiaofei, WEI Xin, CHENG Congcong, REN Xiaoyu, WANG Sichu
Potential hazard assessment of slope farmland soil erosion in black soil region of northeastern China
[Background] Soil depth with rich organic matter provides nutrients for grain production in the black soil region of northeastern China. However, at present, the thickness of the black soil layer in the black soil region of northeastern China is thinner or even lost. A large number of ephemeral gullies and permanent gullies have directly affected the sustainable use of black soil resources and national food security. Classification Standard for Potential Hazard of Soil Erosion (SL718—2015) issued by the Ministry of Water Resources (MWR) focusing on vegetation recovery may not be suitable for assessing slope farmland soil erosion risk. [Methods] Total 196 soil profile samples from slope farmland were collected in Songnen black soil region with area of 200 000 km2, and top soil depth for each sample was identified using quantitative index of mollic epipedon and isohumo features in Chinese soil taxonomy. According to the standard SL718—2015, the erosion risk was assessed for 196 samples using single index of anti-erodibility duration and combined index of vegetation recovery duration and slope degree respectively. Furthermore, they were assessed again by using modified values of anti-erodibility duration for each class based the rate of black soil formation. [Results] The anti-erodibility duration index could be used for assessing the potential hazard of soil depth decreasing caused by soil erosion. However, to maintain the crop growth and farmland productivity, it was better to change the value of threshold soil depth for estimating anti-erodibility duration from 10 cm to 20 cm. According to the standard SL718—2015, only 13.8% of the total 196 samples demonstrated potential hazard by using the index of anti-erodibility duration, and all the samples were classified as light, medium, and heavy potential hazard by using combined index of vegetation recovery duration and slope degree, of which 84.7% was light. The potential hazard degree was underestimated and the standard was not suitable for assessing the soil erosion potential hazard for the slope farmland. [Conclusions] To maintain the sustainable productivity of the black soil, the soil erosion rate should be less than or equal to soil formation rate, which could be used as the critical value for identifying soil erosion risk. The modified threshold values of the anti-erodibility duration for each potential hazard class were suggested as 2 000 years for not potential hazard, >500-2 000 years for light, >100-500 years for medium, >50-100 years for heavy, and ≤50 years for extreme potential hazard. Of total 196 samples, 36.7%, 36.2%, 5.1%, and 14.3% were light, medium, heavy, and extreme potential hazard under modified index class threshold values, i.e., the percentage over light potential hazard was 92.3%.
2020 Vol. 18 (6): 105-114 [Abstract] ( 295 ) [HTML 1KB] [PDF 5072KB] ( 519 )
115 YIN Xiaolin, CHENG Chen, DING Guodong, ZHANG Xiaoming, GAO Guanglei, BAO Shengzhi
Improvement and effects of calcium-containing wastes on saline-alkali soil and growth of Lespedeza bicolor Turcz.
[Background] Saline-alkali soil is widely distributed in our country, while desulfurized gypsum, citric acid slag and fly ash are produced and accumulated in large quantities, which cause great pressure on national economy and ecological environment. But all of them can be used to improve saline-alkali soil. Exploring the improvement of saline-alkali soil by these calcium-containing wastes and the effect on plant growth is conducive to reducing environmental pollution and eventually provides scientific basis for the recycling and reuse of calcium-containing wastes and the improvement of saline-alkali soils. [Methods] Conditional control method was used in the research. Three kinds of calcium-containing waste materials (desulfurized gypsum, citric acid slag and fly ash)were applied to pot-planted Lespedeza bicolor Turcz. with saline-alkali soil soils respectively. Indexes of plant biochemical and soil composition such as net photosynthetic rate Pn, stomatal conductance Gs, transpiration rate Tr, intercellular CO2 concentration Ci, stomatal limitation Ls, water use efficiency (WUE), chlorophyll, content of main ion, exchangeable sodium percentage and sodium adsorption ratio were measured accordingly. [Results] 1) The main soil ion content after improved such as Na+, CO32-, and HCO3- reduced significantly, while the content of Ca2+, Mg2+, SO42- and CEC increased. 2) Na+ and alkaline ions were replaced, and the content of exchangeable Na+ even decreased by 84.3% in desulfurized gypsum treatment. 3) The alkali-reducing degree of each treatment soil exceeded 50%, and the soil was transferred from moderate saline to mild saline-alkali,the degree of salinity in each treatment also shifted from moderate to mild, all of the pH after the experiment decreased, and especially the citric acid residue treatment even reached to 7.1, which was basically neutral. 4) Pn, Gs, Tr and WUE of L. bicolor Turcz. were all higher, while Ci and Ls were lower.5) The contents of chlorophyll a, chlorophyll b and total chlorophyll were all over 2.4 mg/g, 1.1 mg/g and 3.5 mg/g in each treatment, that in fly ash treatment was the highest, mainly because the salt resistance was coupled, meanwhile it showed that by changing salt stress, calcium-containing materials changed the external environmental factors, and then affected the synthesis of plant chlorophyll. [Conclusions] Calcium-containing wastes such as desulfurized gypsum, citric acid slag and fly ash may improve the physicochemical properties of the saline-alkaline soil by changing the composition and contents of salt-damaging ions in saline-alkali soil. Normal physiological functions are maintained by adjusting the feedback regulation mechanism of L. bicolor Turcz. under salt stress, and reducing the effect of salt stress on the growth of L. bicolor Turcz. This study may provide scientific basis and reference for the recycling and reuse of calcium-containing wastes and the improvement of saline-alkali soil.
2020 Vol. 18 (6): 115-122 [Abstract] ( 320 ) [HTML 1KB] [PDF 957KB] ( 429 )
 
Development Studies
123 WANG Xin, ZHU Xuchao, LIANG Yin, TIAN Zhiyuan
Effects of new polyurethane material (W-OH) on infiltration and runoff and sediment yield of two typical erodible soils in South China
[Background] The new polyurethane material (W-OH) has been widely used in soil and water conservation in our country, but its related theories lag behind its practice. Therefore, the study chose the two typical erosion soils red clay of slope cultivated land and arenosol of collapsing gully as objects and analyzed their infiltration and water-sand characteristics under the spraying of different W-OH concentrations. [Methods] Studying how much the new W-OH material influences the typical southern erosion soil in the infiltration, runoff and sediment was conducted. by indoor infiltration experiments and outdoor artificial simulated rainfall tests. [Results] 1) The nutrient of red clay soil and collapsing gully soil was infertile. The content of sand, powder and clay soil in red clay was almost equal. The content of sand in collapsing gully soil was more than 2/3, and the content of clay was only about 5.4%. 2) The spraying W-OH obviously reduced the infiltration rate of the two kinds of soils. With the increasing concentration (0-7%), the average infiltration rate of the red clay soil decreased from 6.98 to 1.42 mm/min and the collapsing gully soil decreased from 5.26 to 2.01 mm/min. The spraying of W-OH had a better effect on reducing the infiltration rate of red clay soil than that of collapsing gully soil. 3) The red clay soil sprayed with 5% W-OH showed an increase of 190% in the average flow rate and a decrease of 73.9% in the rate of sediment yield. The collapsing gully soil sprayed with W-OH showed similarly an increase of 37.3% in the average flow rate and a decrease of 62.1% in the rate of sediment yield. The spraying of W-OH increased runoff and decreased soil loss obviously. 4) The spraying of W-OH presented an inconspicuous impact on the average moisture content of the two kinds of soils before, after rainfall and 24 h later. [Conculsions] This study may provide a theory basis for W-OH's further application to the control of water loss and soil erosion in arable land of southern slope and collapsing gully.
2020 Vol. 18 (6): 123-131 [Abstract] ( 420 ) [HTML 1KB] [PDF 962KB] ( 356 )
 
Forum
132 HU Gang, SHI Xingjun, SONG Hui
Spatiotemporal coupling analysis of precipitation field based on REOF and ESMD: A case study on winter precipitation in Shandong province
[Background] The precipitation in winter has an important influence on soil moisture, winter crops,spring plowing and sowing. Shandong is a major agricultural province in China. However the characteristics of spatio-temporal distribution of winter precipitation in Shandong province is still unclear. The purpose of this study is to reveal the spatio-temporal distribution of winter precipitation and its relationship in Shandong province. [Methods] The data required for the paper comes from China National Meteorological Information Center, and the minimum time scale for data monitoring is 12 h. Based on the methods of both Rotated Empirical Orthogonal Function (REOF), Extreme-Point Symmetric Mode Decomposition (ESMD) and precipitation data from China National Meteorological Information Center, the spatial mode and cycle characteristics of winter precipitation field in Shandong province in recent 68 years were analyzed. [Results] 1) According to analysis of EOF reflecting the spatial variability of the whole region, the winter precipitation in Shandong province presents three main distribution modes: overall consistent, northwest-southeast antiphase and northeast-southwest antiphase. And variance contributions of three modes from EOF were 68.7%, 10.39% and 6.38% respectively. Obviously the first mode, overall consistent one of winter precipitation, was the most important distribution pattern. 2) Based on regional characteristics from REOF analyses, winter precipitation in Shandong province has formed a spatial distribution structure with the high-load areas of southeastern Shandong, northern Shandong and western Shandong respectively. The variances of the three modes were 34.17%, 30.20% and 21.10% respectively, indicating that the winter precipitation anomalies in these three regions had relatively obvious regional characteristics. The results of the period analysis based on FFT (fast Fourier transform) indicated that time coefficients (TCs) of southeast mode had the significant periodic characteristics with quasi-2.9-year and quasi-11.6-year, TCs of the north mode with quasi-2.52-year and quasi-8.29-year, TCs of the west mode with quasi-3.63-year, quasi-6.44-year and quasi-14.50-year. Meanwhile, the trend components of each mode decomposed by ESMD showed that the inter-decadal fluctuation was dominant, and there was no obvious trend of linear change, which indicated that the winter precipitation of the three modes in Shandong didn’t show a single trend characteristic during the monitoring period. Further analysis shows that the southeastern type shows a weak fluctuation and non-significant increase trend, while the northern type showed a weak fluctuation and insignificant decrease trend, while the western type shows little overall change. [Conclusions] REOF and ESMD are effective methods to analyze the spatiotemporal coupling relationship of large scale regional meteorological data. Taking winter precipitation of Shandong province as an example with the above two methods, the research results may provide reference for scientific practice for the rational planning and guidance of agricultural production in Shandong province.
2020 Vol. 18 (6): 132-139 [Abstract] ( 438 ) [HTML 1KB] [PDF 901KB] ( 494 )
 
Review
140 LIU Ran, YU Xinxiao, CAI Qiangguo, SUN Liying, FANG Haiyan, JIA Guodong, HE Jijun
Research progressin the effect of slope length on slope erosion, transportation and deposition processes
[Background] Slope length is one of the important geomorphological factors that affect the process of slope runoff erosion and sediment production. It determines the variation of slope water flow energy along the way, and affects sediment carrying capacity of the water flow, thereby affecting the process of soil erosion, transportation and deposition. In recent years, the research on impact of slope length on soil erosion has received considerable attention. Meanwhile, understanding the changing law of critical slope length provides an important theoretical basis for the study of sediment transport and deposition processes on slopes. [Methods] Based on the literature review, we summarized the influence of slope length on runoff erosion and sediment yield, the general law of erosion critical slope length, the calculation method of critical slope length and the influence of slope length on slope deposition. And we discussed the limitations of soil erosion in terms of slope length, and highlighted the focus of future research. The information for the methods comes from 46 core papers out of 2199 papers published in the web of science, CNKI, Baidu Academic and Science Direct in the past few decades with the keywords of "slope length soil erosion" and "slope surface deposition". [Results] 1)The relationship between slope length and soil erosion is very complicated. Due to the difference in experimental conditions, the erosion intensity varying with slope length has three dynamic forms: increasing, decreasing and fluctuating. 2) Through previous studies, we summarized the definition of the critical slope length for erosion, and pointed out that different critical slope lengths are obtained in different studies due to factors such as rainfall conditions, slope, and slope length. Moreover, the established calculation model of critical slope length is based on the experimental data of researchers, which causes certain limitations. 3)During the erosion, transportation, and deposition of the slope, the sediment is characterized by alternating strong and weak spatial changes. The existence of the critical slope length makes the influence of slope length on slope erosion and deposition more complicated. When the slope length does not reach the critical slope length, erosion and sedimentation activities cannot be fully developed.4)The key points of future research are described as follows. First of all, it is necessary to carry out further research and experiments on the sediment deposition process on the slope. Second, research on the critical slope length for erosion changes as well as experimental research on the relationship between slope lengths of different soil textures and soil erosion should be strengthened. Finally, slope length affects the wave form of slope erosion-sedimentation, and the coupling mechanism of slope length and slope erosion and sediment deposition process needs to be studied. [Conclusions] This paper summarizes the research progress and future research directions of slope length on slope erosion, transportation and deposition process, and aims to provide guidance for the research application and decision-making of soil erosion on slope length.
2020 Vol. 18 (6): 140-146 [Abstract] ( 457 ) [HTML 1KB] [PDF 975KB] ( 584 )
147 CUI Xianghui, QUE Xiao'e, YANG Liu
Current status and thoughts on international standardization in the field of mitigating land degradation and combating desertification
[Background] Land degradation and desertification are the major global ecological issues threating the human living environment and development. The study and formulation of relevant international standards and their application will contribute to the efficient and orderly implementation of land degradation and desertification control at the global, national and regional levels. [Methods] The paper briefly reviews the current status and prevailing trend of global land degradation and desertification, analyzes the today’s development of international standardization in land degradation and desertification control, and summarizes the development processes and achievements initiated by the International Standardization Organization (ISO) from sorting out standardizations in land degradation and desertification control by studying a large number of literatures. Based on achieving the global goal of "zero growth in land degradation" and fulfilling international conventions, the necessities to initiate the development of international standardization in the field of land degradation and desertification control were discussed. [Results] 1)There is an urgent need to establish international standards of terminology, methods, techniques and management to further guide action and planning to combat land degradation and desertification on global scale.2)Based on the global requirement and national priority potential in the field of land degradation and desertification control in China, concrete efforts and measures are proposed to promote the development and further initiatives to launch the international standardization in the field of land degradation neutrality and desertification rehabilitation, such as improving the standard system, cultivating standard talents, service One Belt and One Road strategy, proposing international standards, and enhancing international influence. 3)The coming new technical committee on land degradation and desertification control (LDC-TC) will effectively carry out closer consultation and strengthening cooperation with UN Convention to Combat Desertification (UNCCD) and relevant international organizations, perfecting international standard system, improving basic standards, proposing international standards, and providing specific and operable technical guidelines for combating land degradation and desertification. [Conclusions] In order to promote the international standardization process, it is proposed to 1) establish a secretariat in China for launching the efforts and development of the international standardization to mitigate land degradation and combat desertification; 2) set up a technical committee on land degradation and desertification control (LDC-TC) under the leadership of ISO to develop work plan and mobilize resources, including scopes, tasks, working mechanism, and goals.
2020 Vol. 18 (6): 147-152 [Abstract] ( 571 ) [HTML 1KB] [PDF 740KB] ( 465 )
中国水土保持科学
 
SSWC Continuously Indexed in the 2023 edition of “A Guide to the Core Journal of China”
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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