中国水土保持科学
中国水土保持科学
 
 
 
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2019 Vol.17 No.5  Published 2019-10-31
  
 
Yellow River Basin
1 LI Min, ZHU Qingke
The response of annual sediment transport in the Yellow River to soil and water conservation in different periods since the middle of the 20th century
[Background] The annual sediment transport in the Yellow River is the expression carrier for soil erosion on the Loess Plateau of the middle reaches of the Yellow River, with an average of 1.6×109 t/year in weak soil erosion control. As of 2015, the comprehensive management measures of soil and water conservation in the Loess Plateau of the middle reaches of the Yellow River reached 260 000 km2, and the degree of governance exceeded 62%. The annual sediment transport volume of the Yellow River has not exceeded 5×108 t/year in more than 10 years, and the minimum volume of the annual sediment transport is <108 t/year. At present, China takes the protection and management of the Loess Plateau area in the Yellow River basin as an important strategic measure,therefore, it is of great practical significance to study the response characteristics and degree of annual sediment transport in the Yellow River to soil and water conservation.[Methods] 22 rainfall factors and soil erosion control factors were selected,and regression analysis was used and the statistical analysis of the annual sediment transport of the Yellow River in 1954 to 2015 was conducted in three periods.[Results] 1) From 1954-1966, only a factor of "July to August rainfall in Hekouzhen-Wubao section" "interpreted" the change of the annual sediment transport of the Yellow River by 78%. 2) During the period from 1967 to 1987, a nonlinear regression model composed of soil erosion control degree and three rainfall factors were selected by stepwise regression. 3) From 1988 to 2015, a factor of "controlled percentage of soil erosion" solely "interpreted" the change of the annual sediment transport of the Yellow River by nearly 80%. The changes of the calculated results in the three periods indicated that the response of annual sediment transport amount to soil and water conservation in the four stations of the Yellow River was from not obvious to significant with the increase of soil erosion control degree. Among them, before 1960s, the annual sediment transport of the Yellow River was insensitive to soil and water conservation. 1960s to 1980s, the effect of soil and water conservation on reducing the annual sediment transport of the Yellow River appeared, the annual sediment transport of the Yellow River responded to the degree of soil erosion control, the degree of soil erosion control was the main factor that causes the fluctuation and decrease of annual sediment transport in the Yellow River.[Conclusions] Since the mid-1980s, soil and water conservation plays a significant role in reducing the annual sediment transport of the Yellow River, The annual sediment transport of the Yellow River has a strong response to the degree of soil erosion control; when the controlled percentage of soil erosion is more than 60%, with a confidence of 95%, the annual sediment transport of the Yellow River is less than 600 million t/year; In recent years, the amount of annual sediment transport reduction by the soil and water conservation has exceeded 109 t/year.
2019 Vol. 17 (5): 1-8 [Abstract] ( 507 ) [HTML 1KB] [PDF 6358KB] ( 507 )
9 ZHANG Peng, WANG Dongmei, DING Cong, LI Ping
Time stability of soil effective moisture in alpine hilly region of Qinghai
[Background] In the semi-arid areas of Northwest China, soil moisture is one of the key factors limiting vegetation growth and ecological restoration. In the study area, the study of alpine inferiority and single species, soil temporal and spatial variability of soil water is beneficial to soil water management and vegetation reconstruction.[Methods] From May 15th, 2018 to August 15th, 2018, the soil moisture content of 55 water points in the small watershed of the Anmentan was measured with a CNC 503B neutron meter, measured every 15 days for a total of 7 times; for four soils the type of soil was sampled with a ring cutter, and the soil moisture characteristic curve was measured by an indoor experimental high-speed centrifuge. Then, the soil water content corresponding to the water potential of -1 500 kPa was obtained on the soil water characteristic curve, which is the soil wilting coefficient. The data analysis was done by classical statistical method and time stability analysis, and the data processing tool adopted SPSS and Excel 2016.[Results] 1) The soil in the study area consumes water during the dry season and replenishes water during the rainy season; the 0-20 cm soil layer shows strong variability, and the effective moisture in 20-100 cm soil layer shows moderate variability. 2) The Spearman rank correlation is basically higher than 0.75, and it shows a very significant correlation. The effective moisture of 20-100 cm soil in the small watershed of the study area has high time stability throughout the observation period. The number of points of probability is more than that of shallow layers, and the change of cumulative probability position is small. 3) The range of variation of effective horizontal deviation of 20-100 cm is -79.84%-129.86%, and its standard deviation is 12.63%-55.62%. The relative deviation of soil effective moisture level and the fluctuation range of standard deviation are gradually reduced, and the effective moisture time stability of sample soil increases with the increase of soil layer thickness; the representative points of each soil layer are selected by relative difference analysis. 4) The determination coefficient R2 is 0.668 2-0.811 7.[Conclusions] The surface soil layer shows strong variability and no time stability and the effective moisture in deep soil layer shows moderate variability and has high time stability. The stability shows a trend related to time. The closer the sampling time is, the larger the correlation coefficient is, and the trend decreases with the increase of time lag. The measuring point 18, the measuring point 29, the measuring point 12 and the measuring point 29 respectively represent the average effective moisture content of the soil in the soil layers of 20-40, 40-60, 60-80, 80-100 cm in the study period.
2019 Vol. 17 (5): 9-17 [Abstract] ( 413 ) [HTML 1KB] [PDF 3117KB] ( 489 )
18 CHEN Yinping, XIA Jiangbao, LIU Junhua
Comparison of soil water characteristic curves of saline-alkali land under different farmland shelterbelts
[Background] The Yellow River Delta is the largest estuarine wetland ecosystem in the warm temperate zone in China. However, rainfall was less and the mineral content in underground water was high, which caused soil salinization and alkalization. In this region, the coordinated adaptation of water between plant and soil is the key issue in agricultural development. Therefore, studying the water retention ability of farmland shelterbelts is very important.[Methods] Three typical plant configuration modes Populus tomentosa forest, Fraxinus chinensis forest and mixed forest (P. tomentosa + F. chinensis) were selected as research object,the methods of drying and cutting-ring were used to study water content and physical properties of soil. The soil water contents under different suctions were measured using a high-speed centrifuge, and the characteristic curve were obtained using the mathematical models of Gardner and van Genuchten. Then, parameters such as soil water characteristic curves, soil water capacity, specific water capacity and soil water retention were compared among different farmland shelterbelts. The RMSE (Root Mean Squared Error) and R2 were used to evaluate the fitting of two models for soil water characteristic curves.[Results] In three farmland shelterbelts in Yellow River Delta, with the increase of suction, the variation of soil water content declined fast (-1.0×105-0 Pa) to slow (-3.5×105--1.0×105 Pa) to steady (-11.0×105--3.5×105 Pa). Specific water capacity decreased monotonously and tended to zero infinitely. Soil water characteristic curves at different soil depths showed a steep trend and strong water loss in low suction range, while they presented a smooth and slow trend, with a high water retention ability in high suction range. The soil water retention ability in the three forests was as follows:mixed forest > P. tomentosa forest > F. chinensis forest. The mean value of R2 and RMSE of van Genuchten model was 0.980 and 0.028, that of Gardner model was 0.999 and 0.002, on the whole, the van Genuchten model was superior to the Gardner model on fitting the soil water characteristic curves, and it was advisable to use the van Genuchten model to fit soil water characteristic curve of farmland shelterbelt in the Yellow River Delta.[Conclusions] We should increase soil water conservation and select drought-tolerant species in the construction of farmland shelterbelts in the Yellow River Delta.
2019 Vol. 17 (5): 18-24 [Abstract] ( 447 ) [HTML 1KB] [PDF 905KB] ( 458 )
25 WANG Li, LIN Sha, LI Yuanhang, CHEN Mengfei, HE Kangning, TONG Guoyan
Relationship between understory vegetation and soil moisture in different forest types in Datong, Qinghai province
[Background] This work is to explore the characteristics of soil water and understory vegetation and their relationship with each other in typical deforestation forests in the alpine region of Qinghai.[Methods] The three typical plantations of Picea crasslia forest, Larix principis-rupprechtii forest and Sabina przewalskii forest in Datong county of Qinghai province were selected as research objects, and the original grassland was used as the control. The characteristics of understory vegetation and the soil moisture characteristics of 0-200 cm soil layer and their relationship with each other were studied through field investigation and laboratory experiments.[Results] 1) The soil moisture in the forest lands of the study area was relatively scarce, and the herbaceous plants under the forests were dominated with dry-land plants such as the Elymus dahuricus, Artemisia sacrorum, Poa annua, etc. The richness and diversity of herbs under the L. principis-rupprechtii forest was the best, followed by the P. crasslia forest. The vegetation characteristics of the S. przewalskii were similar to those of the grassland. 2) The average moisture content of different forest types and grassland was in descending order P. crasslia forest (23.79%), grassland (21.29%), S. przewalskii forest (19.02%), and L. principis-rupprechtii forest (16.93%). 3) For topsoil (0-20 cm), the water-holding capacity of forest land was better than that of barren grassland. In 20-60 cm soil layer, the water-holding ability of P. crasslia forest land was the best, and the water-holding capacity of L. principis-rupprechtii forest land was the worst. The effect of vegetation types on soil water-holding capacity increased with increasing soil depth. 4) There was a significantly positive correlation and negative correlation between the species diversity of understory vegetation and biomass and the soil moisture content of the forest(P<0.05), respectively. And the degree of mutual influence decreased with the increase of soil depth, but its effect was mainly concentrated on the soil moisture of 0-120 cm soil layer.[Conclusions] P. crasslia can be used as the main afforestation species for constructing water conservation forests; L. principis-rupprechtii can be used as the main forest tree species for constructing soil and water conservation forests in areas where soil moisture is relatively scarce; the vegetation characteristics of S. przewalskii are close to wild grassland, then S. przewalskii can effectively form a forest and grass composite structural system. L. principis-rupprechtii and S. przewalskii can be used as the main tree species for vegetation construction in the region, and the introduction of local species can be taken into account, thus accelerating the process of vegetation restoration, helping to maintain a virtuous cycle of ecosystems through afforestation and improving the ecosystem of the goal of the service function.
2019 Vol. 17 (5): 25-35 [Abstract] ( 598 ) [HTML 1KB] [PDF 1016KB] ( 477 )
 
Foundamental Studies
36 LU Chuanhao, DONG Xianyong, TANG Jialiang, LIU Gangcai
Impacts of large cascade reservoirs on runoff and sediment load variations in Jinsha River Basin
[Background] The Jinsha River is an important basin in the upper reaches of the Yangtze River. In recent years, many cascade reservoirs have been built in the basin, but the effects of these reservoirs on the variation of runoff and sediment load are not very clear. This study aims to explore the temporal and spatial variation characteristics of runoff and sediment load in study area.[Methods] The data of runoff and sediment load from year 1965 to 2016, and the data of reservoir erosion and siltation in recent years measured by China Three Gorges Corporation, and combined with the method of Mann-Kendall trend test, etc., were applied to analyze the characteristics of runoff and sediment load.[Results] The output of runoff and sediment load in the upper and middle reaches of Jinsha River Vasin was on the rising tendency, after 1998, its annual runoff and sediment increased by 15.27% and 5.01% respectively, indicating that soil and water conservation in these areas needed to be strengthened. The section between Panzhihua and Baihetan (excluding the Yalong River) was the main sediment producing area on the Jinsha River basin, its sediment output accounted for 36.40% of total, and thus this area was the core area when considering sediment load control. Sediment output in the downstream was obviously reduced, its annual sediment decreased by 38.55% after 1998, which was mainly attributed to the construction of the 4 giant cascade reservoirs, meanwhile, the soil and water conservation projects also produced a certain sediment reduction effect.[Conclusions] Our results show that the spatial and spatial and temporal variation variation of runoff and sediment load in Jinsha River Basin are complicated, and the contribution of large cascade reservoirs to the reduction of sediment transport of Jinsha River is over 95%.
2019 Vol. 17 (5): 36-43 [Abstract] ( 536 ) [HTML 1KB] [PDF 1918KB] ( 467 )
44 ZOU Xinyu, ZHANG Zhuodong, WU Mengyao, WAN Yuanqiang
Spatial variability of particle size distribution at slope scale in Bashang region of Hebei province
[Background] Particle size distribution (PSD) is one of the most important properties of soil, and its spatial variability is important for soil erosion modeling and soil and water conservation planning. Previous studies mainly focused on the spatial variability of PSD at large scales and paid little attention to it at small scales. However, the spatial variability of PSD at small scales is an important and undissolved problem as it can effectively refine soil and water conservation practices. Bashang area is a typical agro-pastoral transition zone with serious soil erosion problem, and the spatial variability of PSD of this area is rarely reported and urgently need to be investigated.[Methods] In this study, PSD at 6 depths (0-5 cm, 5-10 cm, 15-20 cm, 25-30 cm, 40-45 cm and 55-60 cm) from 32 sampling points which were located at different slope types and positions in a slope of Bashang area, Hebei province was determined by pipette method. Spatial variation of PSD was analyzed using geostatistics and spatial interpolation for each depth, and the vertical variation of PSD was also analyzed. Soil texture was determined based on the PSD, and its spatial variability was also investigated. The main influencing factors of the spatial variability of PSD and soil texture at slope scale were discussed.[Results] The results show that the spherical model and Gaussian model could be used to describe the semi-variograms of sand, silt and clay particles at all depths. Most of sand, silt and clay particles at most depths have a strong spatial autocorrelation at this slope scale. The sand particles in convex slope, upper slope and central slope are high, while the silt and clay particles are the opposite. With the increase of soil depth, the sand particles tend to increase, the silt particles tend to decrease, and the clay particles are relatively stable. Furthermore, the spatial variation intensity tends to increase with depth as well. There are totally five soil texture types in the slope including clay loam, silt clay loam, loam, sand clay loam and sandy loam, and the main soil texture is clay loam. The spatial variability of soil texture is strong at convex slope and deep layer. Topographic factors including slope position and slope type affect the intensity of soil erosion and lead to the redistribution of soil particles in the slope. Sand particles are less easily to be eroded, thus they are higher in the convex slope, upper slope and central slope.[Conclusions] Slope position and slope type are the main factors that influence the spatial distribution of PSD at slope scale. The number of soil texture types at slope scale is almost equal to that of large scale, and this verifies the importance of the study on spatial variation of soil texture at small scale. Such studies can provide important information for more reliable soil mapping and more precise land management.
2019 Vol. 17 (5): 44-53 [Abstract] ( 385 ) [HTML 1KB] [PDF 7045KB] ( 360 )
54 CHEN Qi, LI Yuanhang, WANG Qionglin, WANG Li, LIN Sha, HE Kangning
Simulation of the daily transpiration process of Larix principis-rupprechtii based on Penman-Monteith model
[Background] Transpiration is the main form of water consumption in vegetation. It is of great significance to study the actual transpiration of forest trees in arid loess area to improve the utilization efficiency of forest moisture, strengthen the construction and management of forest vegetation and maintain the stability of forest branches. Analysis of its evapotranspiration water consumption characteristics also has important guiding significance for regulating the relationship between water and solving the contradiction between water supply and demand in arid regions.[Methods] This paper takes the Larix principis-rupprechtii in the loess arid area of Qinghai province as the research object. From May to August 2018, the real-time data of the stem sap flow (10 min frequency) of Larix principis-rupprechtii growing season was obtained by using the probe stem flow meter, combined with the Penman-Monteith equation. The inverse total pore resistance γst of the canopy and the meteorological data obtained from the portable automatic weather station were used to construct the regression model of γst and meteorological factors of Larix principis-rupprechtii in the alpine region, which provided a basis for accurately estimating the transpiration of L. principis-rupprechtii. It provides scientific reference for the accurate estimation of transpiration of L. principis-rupprechtii.[Results] 1) The diurnal variation of transpiration rate of L. principis-rupprechtii shows a single peak curve, and of meteorological elements for sap flow is about 70 min. 2)The canopy layer stomatic resistance at different periods was negatively related to VPD and temperature T, and is positively related to air relative humidity RH. By comparison, we can find that the effect of multiple factors regression of meteorological factors is better than that of single factors regression. The simulated results are ideally within an average error of 14.5%.The multivariate regression equation between γst and three meteorological factors during the period from 00:00 to 8:00 is γst=-117 376.512+103 310.241VPD-3 134.50t+1 608.292RH. The multivariate regression equation for the period from 08:00 to 20:00 is γst=-269.467+244.359VPD-20.451t+8.033RH. The multivariate regression equation for the 20:00-24:00 period is γst=-1 570.795-141.384t+49.334RH. The multivariate regression model established by this method can simulate the transpiration process of L. principis-rupprechtii in high cold area and provide reference for studying transpiration of vegetation.
2019 Vol. 17 (5): 54-64 [Abstract] ( 546 ) [HTML 1KB] [PDF 1185KB] ( 491 )
65 LI Yexin, Lü Gang, WANG Daohan, LI Chaohui, SONG Ge, DU Xinpeng, DONG Liang
Analyzing the saturated hydraulic conductivity of surface soil in a dump by three measuring methods
[Background] Domestic and foreign scholars have conducted a lot of researches on the selection and adaptability of reclaimed vegetation, infiltration characteristics and hydrological effects of reclaimed mine soil, water-holding capacity of soil, and the restoration of soil fertility in the dump. However, it is lack of study on the saturated hydraulic conductivity of reclaimed soil with different reclaimed vegetations in the dump. The saturated hydraulic conductivity of reclaimed soil has an important impact on the formation of surface runoff and soil erosion in the dump, and it is of great significance to understand the soil water movement and the characteristics water leakage in this area. At present, there are many methods for determining the soil saturated hydraulic conductivity of a dump, but the accuracy of the measurement results needs to be improved.[Methods] In the present study, saturated hydraulic conductivity of surface soil with 3 types of reclaimed vegetations (Robinia pseudoacacia forest land, Ulmus pumila forest land, and weeds) was measured and calculated by indoor-ring infiltration method, double-ring infiltration method and Hood infiltrometer, and 3 samples of every forests sample plot were taken. The soil water content, bulk density, porosity and gravel content were measured indoor and their effects on saturated hydraulic conductivity were analyzed. Saturated soil hydraulic conductivity of surface soil in the reclaimed soil was evaluated by analytic hierarchy process. The differences and its reasons of the results by indoor-ring infiltration method and double-ring infiltration method were clarified, and the optimal method of saturated water conductivity was discussed.[Results] 1) Soil moisture content with different reclaimed vegetations was 13.51%-15.48%, and soil bulk density was R. pseudoacacia forest land > weeds > U. pumila forest land. The soil organic matter was 6.17-8.05 g/kg. The gravel content of R. pseudoacacia forest land, U. pumila forest land and weeds were 52.39%, 47.52%, and 54.03%, respectively. The sand content of three reclaimed vegetations was 36.80%-41.43%, silt content was 48.87%-54.27%, and clay content was 8.30%-9.70%. 2) The soil saturated hydraulic conductivity increased significantly with the increasing reclamation years, which was due to the improvement of soil structure by vegetation restoration. The surface soil saturated hydraulic conductivity of R. pseudoacacia forest land, U. pumila forest land, and weeds were 0.77, 0.54, 0.48 mm/min, respectively, and there was no significant difference among three reclaimed vegetations (P>0.05). 3) The results of different measurement methods were Hood infiltrometer < double-ring infiltration method < indoor-ring infiltration method, and the accuracy of Hood infiltrometer was the highest. 4) The saturated hydraulic conductivity was a significant positive correlation with gravel content and silt content, and was a significant negative correlation with bulk density and clay content. The water conductivity of surface soil in the dump was U. pumila forest land (0.523) > R. pseudoacacia forest land (0.501) > weeds (0.488).[Conclusions] The soil saturated hydraulic conductivity is shown as follows U. pumila forest land > R. pseudoacacia forest land > weeds. The results of soil saturated hydraulic conductivity measured by the three methods differed. The dispersion degree and error of the results measured by Hood infiltrator are less than those measured by indoor-ring infiltration method and double-ring infiltration method, there is no need to disturb soil and no head pressure, which is more in line with the actual process of soil water infiltration. Hood infiltrometer shows better applicability in measuring surface soil saturated hydraulic conductivity.
2019 Vol. 17 (5): 65-74 [Abstract] ( 437 ) [HTML 1KB] [PDF 1504KB] ( 387 )
 
Applied Studies
75 LOU Yibao, SHI Dongmei, JIANG Guangyi, JIN Huifang, CHEN Zhengfa, LIN Zi
Evaluation of soil quality in the cultivated-layer of sloping farmland in purple hilly area based on minimum data set
[Background]The soil quality of a plowing layer directly affects the productivity of sloping farmland, in order to accurately evaluate the soil quality characteristics of a plowing layer for purple sloping farmland, objectively evaluate the soil quality in the plowing layer of purple soil sloping farmland is an important basis for preventing the soil erosion and degradation of purple soil sloping farmland and ensuring the high efficiency and stability of the soil productivity in plowing layer.[Methods] The plowing-layer (0-20 cm) soil of purple sloping farmland of Chuxiong-Yunnan, Guilin-Guangxi, Xingguo-Jiangxi and Nanxiong-Guangdong were collected as the research objects. The minimum data set (MDS) was established and the cultivated-layer soil quality was evaluated by the combination of principal component analysis (PCA) and correlation analysis based on the 12 soil property indexes which were selected.[Results] 1)Soil quality of cultivated-layer for sloping farmland varied significantly among different purple soil sites. Soil nutrients of cultivated-layer were poor relatively, soil organic matter (14.89 g/kg) and total nitrogen (0.85 g/kg) were on the fourth level, and available phosphorus (28.84 mg/kg) on the secondary level of the classification criterion of soil nutrient, pH value was faintly acidity. The ranges of soil bulk density was 0.93-1.62 g/cm3, and the cultivated-layer thickness varied of 15-30 cm, The variability of soil bulk density, silt content, cultivated-layer thickness, pH value variability were small. Sand content, penetration resistance, shear strength and total nitrogen with general variability, and the clay content, saturated water conductivity, organic matter and available P were in large variability. In general the variability of soil chemical indexes were greater than that of physical indexes. 2)The MDS on soil quality evaluation included the seven indexes of soil bulk density, available phosphorus, organic matter, saturated hydraulic conductivity, penetrate resistance, sand content and cultivated-layer thickness, which reflected the effective information of soil quality of cultivated-layer with accuracy evaluation result for soil and water conservation fertilizer conservation and yield-increasing potential. 3)The soil quality of cultivated-layer for purple sloping farmland was ordered as Chuxiong-Yunnan > Guilin-Guangxi > Xingguo-Jiangxi > Nanxiong-Guangdong. The obstacles of cultivated-layer with low penetrate resistance and soil bulk density in Chuxiong-Yunnan, lower organic matter and cultivated-layer thinning were the obstacles of cultivated-layer for Guilin-Guangxi and Nanxiong-Guangdong seperately, Xingguo-Jiangxi with the obstacle of slightly higher sand content and lower saturated water conductivity.[Conclusions]The results may provide some useful scientific supports not only for the soil quality recovery of the cultivated-layer but for the sustainable utilization of crop growth and the control of soil and water loss of purple soil sloping farmland,which are also conducive to soil improvement, reasonable cultivated layer construction and sustainable utilization of the sloping farmland recourses in purple hilly area.
2019 Vol. 17 (5): 75-85 [Abstract] ( 561 ) [HTML 1KB] [PDF 3142KB] ( 321 )
86 LIU Linqi, LI Yang, WANG Qian, CHEN Jingling, YANG Xitian, FAN Wei
Dynamic characteristics of Quercus variabilis seedling growth
[Background] Plant growth dynamics reveals the impacts of the environment on plants. Quercus variabilis is one of the afforestation species widely used in rocky mountainous areas. It is prone to growth retardation or death under environmental stress. In order to further reveal the reasons for the stunted seedling growth and death, this paper traced the life course of each organ.[Methods] In this study, the seedlings of Quercus variabilis were sampled by hand-excavation in the nursery field. The sampling interval was 10 d in the first year, one month in the second year, and one season in the third year, and the growth, dry biomass and sugar concentration of every organ in the seedlings were measured by drying and Anthrone colorimetry.[Results] 1) During the first growing season, there was obvious growth-stasis-regrowth of stem and leaf, showing the phenomenon of blocked growth in summer.2) Except for the winter season (December-March of the next year), the roots of 1/2-year-old seedlings grew continuously. At the age of 3, the rate of root elongation was slower than at 1/2 years, with root thickening and lateral root growth being the main growth.3) Analysis of seed kernel dry matter consumption and total sugar concentration showed that the growth of seedlings in their first summer (from early June) was blocked, which was in line with the lowest seed kernel residue and total sugar. 4) In early June, the total sugar concentration of the seed kernel began to fall beneath the total sugar concentration of the leaf, indicating that the seed kernel was no longer the main nutrient donor of the plant.5) Seedlings aged 2 to 3 years began to grow from the middle of March, and growth slowed down in July, and they did not show the phenomenon of blocked growth.[Conclusions] The ecological strategy of 0-3 years old seedlings of Q. variabilis was to ensure the growth of the main roots, the 1-year-old seedlings have stunted growth in summer, which is closely related to the period of weakest seedling resistance transform (heterotrophic autotrophic transformation), and there was no stagnation in the growth of 2 or 3 year old seedlings.
2019 Vol. 17 (5): 86-92 [Abstract] ( 424 ) [HTML 1KB] [PDF 4761KB] ( 586 )
93 MUHADAISI Ariken, MAMAT Sawut, YIKELIMA Abudoumiti, MA Chunyue
Spatial distribution characteristics of surface water quality in the Ugan-Kuche river oasis
[Background]Water resources have become a global issue, especially in arid and semi-arid regions, where water resources are scarce and water quality is deteriorating.However, there are few studies on the spatial distribution of surface water quality in typical arid areas(Ugan-Kuche river oasis), thus the objective of this work is to study the spatial and temporal distribution characteristics of surface water quality in Ugan-Kuche river oasis.[Methods] The water quality indexes of the sampling points were taken as the research object, and the water quality variations in 2016-2017 were compared and analyzed by descriptive statistical methods, and the water chemical type was judged by combining the Piper diagram, the time trend of surface water chemistry characteristics were analyzed by GIS and statistical methods.[Results] 1)The river water quality indices such as pH, EC(Electrical Conductivity), TDS(Total Dissolved Solids), Cl-, Ca2+, K+, and Mg2+ in 2016 were higher than in 2017, but SO42-, HCO3-, Na+ concentration in 2017 were higher than in 2016. 2) The sampled water chemistry also showed the similar spatial variations, mainly expressed as Cl-SO4-Na-Mg、Cl-SO4-Ca-Mg and HCO3-Cl-SO4-Na-Ca-Mg.The dominant mechanism of natural control of surface water chemical sources was the evaporation concentration type. 3) The river water quality indices such as EC, Ca2+, Na+, Mg2+, Cl-, and SO42- showed a similar stripped distribution pattern. The value of each parameter showed an increasing trend in the upstream to downstream process.[Conclusions] From the spatial scale, the main reason for the surface water quality in the middle and lower reaches of Kuche River is that the natural factors such as the terrain of north high and south low of the study area and the human factors exacerbate the degree of salinization, which destroys the ecological environment. From the time scale, the water-salt stress is becoming more and more significant due to the lack of water and soil resources and the unreasonable use of human and soil resources in Ugan-Kuche river oasis.
2019 Vol. 17 (5): 93-99 [Abstract] ( 558 ) [HTML 1KB] [PDF 4773KB] ( 469 )
100 LI Zedong, LI Yiran, ZHOU Xiaoying, ZHANG Ruming, CHENG Tiantian, ZHANG Yongtao
Drought resistance evaluation of three afforestation tree species in lithoid hilly area of North China
[Background] The soil in the lithoid hilly area of North China is poor and the soil erosion is serious, which severely restricts the productivity of these undeveloped mountains. Vegetation restoration is an important measure in recovering ecological environment. A large number of studies have shown that when plants are subjected to drought stress, a series of physiological changes will be produced in plants to adapt to drought stress, but the response characteristics, adaptability and physiological mechanisms of different plants to drought stress vary. Therefore, studying the response characteristics and physiological mechanisms of different tree species under drought stress has important practical significance for its application in barren hills greening and vegetation restoration.[Methods] Using the test method of potted water control, 10 2-year old plants and consistent Fraxinus chinensis, Quercus acutissima and Gleditsia sinensis seedlings were selected as test materials, and their photosynthesis parameters, MDA content,cell membrane permeability,relative water content, leaf chlorophyll content, SOD activity, and proline content in response to drought stress under continuous drought conditions were determined. The relationship between each physiological index and drought resistance was compared by grey relational analysis, the drought resistance of three tree species was comprehensively evaluated by membership function method.[Results] 1) With the drought increasing, the MDA content, membrane permeability and SOD activity of three tree species increased, while the relative water content and net photosynthetic rate of leaves decreased, and the chlorophyll content of Q. acutissima increased. 2) The proline content of the G. sinensis was greatly increased, and the proline content of the F. chinensis and Q. acutissima remained substantially unchanged. The drought resistance of three tree species under moderate or severe drought stress was ranked by membership function method, the results showed as G. sinensis > Q. acutissima > F. chinensis. 3) Grey correlation analysis showed that the correlation between the indexes of moderate drought conditions and drought resistance was as follows:leaf relative water content (0.784) > SOD activity (0.723) > chlorophyll content (0.652) > cell membrane permeability (0.527) > MDA content (0.526) > net photosynthetic Rate (0.506) > proline content (0.503). The correlation between various indicators and drought resistance in severe drought conditions was as:leaf relative water content (0.749) > cell membrane permeability(0.632) > net photosynthetic rate(0.563) > SOD activity (0.543) > MDA content (0.528) > chlorophyll content (0.508) > proline content (0.506).[Conclusions] The three tree species have certain commonality in the means of resisting drought, that is, to prevent drought stress by maintaining the leaf water and SOD to eliminate free radicals and reducing the degree of lipid membrane peroxidation. This research can distinguish the differences between different physiological indicators in the drought stress of plants and screen the drought-resistant tree species to provide reference for the selection and ecological restoration of afforestation species in the lithoid hilly area of North China.
2019 Vol. 17 (5): 100-109 [Abstract] ( 496 ) [HTML 1KB] [PDF 921KB] ( 378 )
110 WU Jie, SHI Mingchang, DING Guodong
On the spatio-temporal pattern of desertification in Zhenglan banner, Hunshandake sandy land
[Background] The development of desertification in Hunshandake sandy land seriously endangers the ecological environment and obstructs the sustainable development of economy, the control of desertification is urgent, it is of great significance to study the changing process and main causes of desertification in order to control desertification. Therefore, taking Zhenglan banner in the hinterland of sandy land as the study area to accurately analyze the process and causes of desertification change in this area would provide the basis for desertification control and ecological environment restoration in Hunshandake sandy land.[Methods] LandsatTM/OLI remote sensing image from 1985 to 2015 in the study area were used to calculate the normalized difference vegetation index and to construct the desertification index based on normalized difference vegetation index, the temporal and spatial variation of desertification index was analyzed using the index classification method,Theil-Sen trend analysis method and Mann-Kendall test method. Then based on the annual precipitation, annual average temperature from 1985 to 2015 in the study area, spearman grade correlation method was applied to analyze the spatio-temporal difference of the driving effect of meteorological factors on desertification. The influence of human activities on desertification was analyzed by using socio-economic data.[Results] 1) The desertification in the study area has expanded and aggravated in the past 30 years, and experienced 4 evolution in the process. From 1985 to 1989,desertification began to expand in the west and the degree of desertification increased; from 1989 to 2000, desertification continued to expand but the severity decreased; from 2000 to 2004, desertification shrank, the degree of desertification alleviated; from 2004 to 2015, desertification was reversed, the degree of desertification increased, and the degree of desertification expanded again. 2) From 1985 to 2015, the dominant trend of desertification in Zhenglan banner was non-significantly changed, its area reached 69.92% of the total desertification,and between the significantly change trends, the upward trend was mainly located in the east, its area reached 18.46%,the downward trend mainly located in the west, its area reached 11.62%. 3) The correlation between climate and desertification is mainly non-significantly correlation in space, which indicated that climate was not the most important influencing factor for the change of desertification in this area,the main factor was human activity.Therefore, the desertification change in Zhenglan banner was the result of the superposition of climate and human activities, especially animal husbandry. there are temporal and spatial differences in the superposition effects of climate and human activities.[Conclusions]The main reason for the increase of desertification in Zhenglan banner in the past 30 years is human activities, thus human activities should be restricted under the current unfavorable climate conditions, so as to achieve the purpose of ecological control.
2019 Vol. 17 (5): 110-119 [Abstract] ( 618 ) [HTML 1KB] [PDF 6160KB] ( 432 )
120 ZHANG Fan, JI Xiaodong, MA Yuanyuan, LI Xinyuan
Physical and mechanical properties and microstructure of black soil modified by natural zeolite
[Background] The black soil area in northeast China is one of the important commercial grain supply areas such as corn and japonica rice. However, studies show that the soil erosion in this area is deteriorating, which seriously affects the fine fertility of black soil, and soil erosion is the main reason for this situation. Therefore, improving the anti-erosion ability of black soil is a necessary means to alleviate the current situation of soil erosion. Physical and mechanical properties and microstructure are the basic properties of black soil, which can indicate its resistance to erosion.[Methods] Natural zeolite used in this study was mainly inclined zeolite. XRF, XRD and SEM respectively were used to determine the main chemical composition of natural zeolite, mineral composition and surface morphology and structure. The black soil was taken from Songliao Plain as the research object. Natural zeolite was mixed into the black soil in the proportions of 0, 5%, 10%, 15% and 20%, and after 60 d of pot culture, triaxial compression test method, ring knife method, mercury injection instrument method were adopted to determine and analyze the mechanical properties, physical properties and microstructure change rules of different remolded soil.[Results] 1) With the increase of dosage of added natural zeolite, the cohesive force of the black soil increased gradually and was positively related with added natural zeolite dosage. Internal friction angle increased more than that of control group with added natural zeolite dosage, but there was no obvious regular pattern. The density of black soil increased gradually and was positively related with added zeolite dosage. Total porosity decreased and negatively related with added zeolite dosage. 2) As the mixing dosage of natural zeolite gradually increased, the microstructure of black soil changed, and the total pore volume showed a decreasing trend. The changes at both ends of each curve showed a slight upward trend of small pores and a slight downward trend of large pores, indicating that the proportion of smaller diameter pores in the black soil increased slightly. 3) Based on the analysis of relevant literature, it is reasonable and economic to select 10% natural zeolite to improve black soil.[Conclusions] Natural zeolite may improve the mechanical properties, physical properties and microstructure of black soil. The changes of microstructure and macroscopic physical properties are consistent with each other, which will lead to the changes of mechanical properties of the black soil and effectively improve the shear strength of the black soil. And this change can be explained to some extent by the internal structure changes of the black soil.
2019 Vol. 17 (5): 120-127 [Abstract] ( 413 ) [HTML 1KB] [PDF 2310KB] ( 341 )
 
Engineering Studies
128 ZHANG Xingyi, QI Zhi, ZHANG Shengmin, LI Hao, DU Shuli, HU Wei, DING Chao, HAN Xing
Rehabilitation engineering of gully filling in the Mollisols farmland of Northeast China
[Background] Gully erosion greatly harms the ability of crop production and agroecosystem due to the loss of arable soil and the obstacle of tractor travel. Gully erosion is a big issue and urgently needed to renovate for the agricultural sustainable development in the Molliosls area of Northeast China.[Methods] An innovative rehabilitation engineering of gully filling in the farmland was set up. The basic design principle was the gully disappearance with the gully body filled by straw and its surface covered by soil. A drainage system consisting of conceal conduit and seepage pit was established under ground. New gully will be not formed in the filled area, and tractors can move freely.[Results] The rehabilitation engineering consists of gully reshaping, conceal conduit laying, straw bundling, straw bundle stacking, surface earthling, earth bund constructing, seepage pit building and exit protecting. The land destroyed by gully erosion was filled and gully disappeared. The stream on the surface of rehabilitation gully got into the conceal conduit through the infiltration of gully surface covered soil and the seepage pit to straw layer, then concentered to the conceal conduit. More than 90% of the converged flow was drained out the field from underground, which greatly decreased the power of water flow and no new gully was formed. Small gully or the brand of median and large gully with the depth ≤ 2 m could be rehabilitated by this engineering. Up to now, over 300 gullies was rehabilitated by the national projects of gully controlling, Mollisols land protecting and territorial controlling in the Mollisols area of Northeast China, and 1.33 km2 farmland was rehabilitated. More than 0.2 million gullies and 1 333 km2 farmland are expected to be rehabilitated by the engineering in the northeast of China. About 0.6 billon kg grains would be increased each year.[Conclusions] The key technology of the gully rehabilitation engineering is to change the surface water flow to the conceal conduit and seepage pit drainage. The optimal gullies for the rehabilitation are formed in the farmland and their depths are <2 m.
2019 Vol. 17 (5): 128-135 [Abstract] ( 594 ) [HTML 1KB] [PDF 3531KB] ( 427 )
136 DUAN Qian, YUE Youzhi, QI Fei, LIU Xia, YANG Xiangwei, LI Jiazuo, YUAN Xigong, YUAN Li
Spatio-temporal distribution and compliance analysis of disturbance patches in production and construction projects
[Background] In recent years, with the development of regional social economy, production and construction projects are increasing day by day. The phenomenon of soil erosion caused by production and construction projects is becoming more and more serious. In order to strengthen overall supervision of production and construction projects, to effectively curb man-made soil erosion, and to ensure the sustainable development of regional ecological environment and social economy, this paper takes Huoqiu county in Anhui province as the research area and explores the spatial-temporal distribution and compliance analysis and evaluation of disturbance pattern spots in production and construction projects.[Methods]Using multi-source data, combined with ArcGIS platform, UAV aerial photography, field survey and other technical means, the disturbance pattern features of production and construction projects in the region were explored.[Results]1)From 2015 to 2016, there were 780 disturbance patches of production and construction projects with an area of >0.1 hectares in Huoqiu county, covering a total area of 8 442.14 hectares. Disturbance pattern spots were concentrated in the northwest and southwest of Huoqiu county. The types of production and construction projects were mainly metal ore mining, and the disturbance pattern area of production and construction projects mainly concentrated in 1-5 hm2, and the main disturbance change type was the continuation pattern. 2)Houqiu county has approved 20 production and construction projects. Well mining Metai ore accounted for 70% of the approved projects. The scope of responsibility for prevention and control of approved production and construction projects involved 51 map spots, among which 12 were in compliance, and the main type was well mining metal ore. There were 39 non-compliant spots, including 16 that were suspected to have changed construction sites, and 23 that were suspected to be beyond the scope of responsibility for prevention and treatment. 3)In Huoqiu county, 580 suspected unapproved map spots with an area of more than 1 hectare accounted for 88.68% of the total number. Most of the projects were not implemented in the production and construction activities, but also highlighted the lack of local supervision and other issues.[Conclusions]The situation and task of water administration department's supervision and management is severe. It is still necessary to strengthen the precise supervision and management of production and construction projects to effectively curb man-made soil erosion.
2019 Vol. 17 (5): 136-145 [Abstract] ( 582 ) [HTML 1KB] [PDF 3541KB] ( 439 )
 
Research Review
146 GUO Zhonglu, CAI Chongfa
Research status and hotspots of biological soil crust based on CiteSpace and HistCite
[Background] Biological soil crust (BSC) is an integral part of ecosystems, playing an important role in soil hydrology, nutrients cycling and stabilizing soils. Summarizing the research trends of BSC in China and abroad would provide reference basis for relevant research.[Methods] CiteSpace and HistCite were employed to explore the number, keywords and research team based on the literatures selected from CNKI and Web of Science core database. In Web of Science,searching pattern was TS=(biological crusts or biological soil crusts or biocrust or moss soil crusts or lichen soil crusts or cyanobacterial soil crusts or algal soil crusts) not TS=(sea or marine or ocean or reservoir or lake or physical soil crusts or salt crusts or bread or aquatic or drug or crystalline lattice) and TS=soil. In CNKI, searching pattern was SU=‘biological crusts’ or SU=‘crust*’ or SU=‘biological soil crusts’ or SU=‘algal crust’ or SU=‘moss crust’ or SU=‘lichen’ or SU=‘mixed algal-moss crust’.[Results] 1) The number of published articles in the field of BSC appeared an overall upward trend. More specifically, USA and China were the top two countries contributing to these articles, while Cold and Arid Regions Environmental and Engineering Research Institute and Xinjiang Institute of Ecology and Geography of Chinese Academy of Sciences were the top two institutions in China. 2) Compared with other countries, China's BSC research started relatively late, but the numbers of articles increased sharply since 2000; further, some research area in China have been hot regions of international BSC research. The composition, succession and seasonal change of BSC and their effects on carbon and nitrogen cycling, soil physical and chemical properties, soil hydrological process and soil erosion, as well as responses of BSC to disturbance were research hotspots. 3) It has formed some core academic teams with LI Xinrong in the Cold and Arid Regions Environmental and Engineering Research Institute of CAS, ZHANG Yuanming in the Xinjiang Institute of Ecology and Geography of CAS, ZHAO Yunge in the Northwest A&F University and BU Chongfeng in the Northwest A&F University, and LIU Yongding in the Institute of Hydrobiology, CAS. Moreover, there was a strong cooperative relationship among three teams of LI Xinrong, ZHANG Yuanming and ZHAO Yunge.[Conclusions] Through summarizing and analyzing research focus issues and research hotspot BSC, it is conducive to researchers to comprehensively understand research history and present situation of BSC at home and abroad.
2019 Vol. 17 (5): 146-156 [Abstract] ( 387 ) [HTML 1KB] [PDF 4586KB] ( 682 )
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
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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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