中国水土保持科学
中国水土保持科学
 
 
 
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2023 Vol.21 No.1  Published 2023-02-28
  
 
Foundamental Studies
1 QIN Qishan, ZHENG Fenli, SHI Hongqiang, WANG Xuesong, WANG Bin, LI Zhi, ZHANG Jiaqiong
Impacts of slope rainfall and inflow in Mollisol region of Northeast China on the soil aggregate loss and particle transport
[Background] Soil loss area on the slope croplands of the Chines Mollisol reached 214 100 km2, accounting for 19.7% of the totle land area. Soil aggregates loss and particle transport is often identified as the main mechanism that leads to nutrient loss. This reduces soil fertility and affects the utilization of Mollisol resources. Thus, to study the effects of rainfall and inflow on soil aggregate loss and particle transport may deepen the understandings of soil degradation processes driven by soil erosion and provide scientific basic for soil resource sustainability.[Methods] This study applied simulated rainfall and inflow experiments to investigate effects of rainfall and inflow on soil aggregate loss and particle transport in a 10° sloping landscape of Mollisol region of Northeast China. The experimental treatment included two rainfall intensities of 50 and 100 mm/h (R50 and R100), one inflow rate of 100 mm/h (I100), and the combinations of rainfall intensity and inflow rate (50 mm/h rainfall intensity + 50 mm/h inflow rate (R50I50), 50 mm/h rainfall intensity + 100 mm/h inflow rate (R50I100), 100 mm/h rainfall intensity + 50 mm/h inflow rate (R100I50)).[Results] 1) Under the same amount of water supply, the sloping soil erosion rate under the R100 treatment was 1.9 and 2.4 times compared with the R50I50 and I100 treatments, respectively; and the soil erosion rate under the R100I50 treatment was 1.3 times compared with R50I100 treatment, which indicated that the effect of rainfall on sloping soil erosion was greater than that of inflow. 2) When rainfall played a dominant role in the process of sloping water erosion, such as the R50, R100, R50I50 and R100I50 treatments, the loss of<0.25 mm aggregates increased by 20.6%, 16.7%, 17.9% and 21.8% respectively, compared with the tested soil. When inflow took a dominant role in the process of sloping water erosion, such as the I100 and R50I100 treatments, the loss of ≥ 0.25 mm accounted for 61.9% and 65.2%, respectively, which demonstrated that the dispersion effect of inflow water on Mollisol aggregates was less than that of rainfall. Moreover, MWD (mean weigh diameter) value could better reflect the characteristics of soil aggregate loss. 3) The total loss of sand and clay particles under the R100, I100 and R50I50 treatments increased by 1.4%-9.5%, compared with the R50 treatment; the proportion of sand particle loss under the R50I100 and R100I50 treatments increased by 0.8%-4.0%, compared with the R100, I100 and R50I50 treatments; and it increased by 3.7%-6.0% compared with the R50 treatment; while the total proportion of silt and clay particles decreased accordingly, indicating that the loss of coarse particles increased with an increase of inflow rates.[Conclusions] The dispersion action of rainfall on Mollisol aggregates was larger than that of inflow and the sorting action of sediment particles in the depended on the action degree of rainfall and inflow in sloping water erosion process.
2023 Vol. 21 (1): 1-9 [Abstract] ( 327 ) [HTML 1KB] [PDF 931KB] ( 214 )
10 SU Yuanyi, ZHANG Yang, YANG Zhi, LI Peng, LI Zhanbin, WANG Tian, ZHANG Naichang
Erosion and sediment particle sorting characteristics of sand-covered loess slope during thawing period
[Background] Soil erosion in the wind water erosion crisscross zone of the Loess Plateau in spring thawing period is usually the result of water erosion, wind erosion and freeze-thaw erosion. However, the problem of soil erosion caused by joint action is far more than the harm of single action erosion itself. The superposition of different erosion types will lead to great changes in soil erosion.[Methods]In order to explore the influence of thawing water erosion on sand-covered loess slopes during the thawing period, 4 types of non-frozen bare slope (U0), non-frozen sand-covered slope (U1), frozen-soil bare slope (F0), and frozen-soil sand-covered slope(F1) were selected. The slope surface (with a thickness of 1 cm of sand cover) was the research object. A 2 m long slope surface and a flow rate of 1 L/min were designed to conduct an indoor water discharge scour test in order to understand the slope erosion process and the separation characteristics of sediment particles.[Results]1) The initial runoff generation time of the frozen-soil slopes (F0 and F1) was significantly shorter than that of the non-frozen slopes (U0 and U1), and the initial runoff generation time of the sand-covered slopes (U1 and F1) was significantly later than that of the bare slopes (U0 and F0).2) The average runoff and sediment yield rates of each slope were U0 < U1 < F0 < F1, and U0 < U1 < F0 < F1. The average runoff and sediment yield rates of U0 were significantly different from those of U1, F0 and F1 (P<0.05). 3) The average value of mean weight diameter (MWD) of sediment particles on each slope was as follows:Loess substrate < F0 < U0 < F1 < U1 < Sandy soil substrate. During the experiment, MWD of the bare slopes fluctuated little with the extension of runoff generation time, and MWD of the sand-covered slope increased and decreased significantly in two processes. Under the condition of erosion, sand and coarse silt were more easily carried away by runoff, and sand was more easily eroded on the sand-covered slopes, while coarse silt was more easily eroded on the bare slopes.[Conclusions]Sand cover on slope results in the delay of the initial runoff generation time, and the delay effect is more obvious with the increase of sediment cover thickness. Froze soil will significantly reduce the initial runoff generation time on the slope. Froze soil will break large soil particles, resulting in the increase of fine particles on the slope.
2023 Vol. 21 (1): 10-18 [Abstract] ( 350 ) [HTML 1KB] [PDF 1661KB] ( 147 )
19 WANG Xuan, DU Shuhan, DENG Limei, ZHU Wanze, LIU Gangcai
Effects of different soil porosity on the water conservation of typical vegetation system in western Sichuan
[Background] Water conservation is one of the important services of the ecosystem, it is closely related to vegetation type and its coverage, litter composition and its quantity, soil layer thickness and soil physical properties, and is a result of the synergistic action of vegetation and soil. But there is no unified standard method to assess its capabilities, and the quantified results of the different methods vary greatly.[Methods] Therefore, taking the Miyaluo forest area of western Sichuan as an example, the total water conservation volume were determined by measuring and calculating the aboveground water retention capacity of typical vegetation and the different porosity constants of its soil. The water conservation capacity of vegetation was determined by water immersion, and the soil porosity constants were determined by soil core samples.[Results] Results showed that the aboveground water conservation capacity of mixed forest was the maximum with the amount of over 100 t/hm2, and then the rank order of the capacity was artificial forest>alpine rhododendron shrub forest>birch forest>coniferous forest>meadow> alpine oak shrub forest > alpine willow shrub forest, which indicates that increasing biodiversity can improve water conservation capacity. The rank order of soil total porosity of different vegetation was coniferous forest> birch forest > meadows > alpine rhododendron shrub forest > artificial forest > alpine willow shrub forest > alpine oak shrub forest > mixed forest. The water conservation capacity within the soils in the study area accounted for more than 90% of the total water conservation capacity, which was consistent with the results of the existing studies. The rank order of soil dehydration rate of different vegetation types was arbor forest> shrub forest> meadows. The difference of soil total porosity was not obvious under different vegetation, but the porosity of capillary and non-capillary were significantly different; the volume of aboveground water conservation of vegetation + water quantity of soil total porosity were not significantly different among various vegetation types, and coniferous and birch forest had the maximum, while mingled forest had the minimum; the volume of aboveground water conservation of vegetation+water quantity of soil non-capillary porosity were significantly different among various vegetation types, and coniferous-forest had the maximum, while meadow had the minimum; but there was opposite trend for the volume of aboveground water conservation of vegetation + water quantity of soil capillary,which was in accord with the results of InVEST model.[Conculsions] The current study suggests that the volume of aboveground water conservation of vegetation in vegetation system + water quantity of its soil capillary porosity is scientific and accurate for assessment the water-holding function of the ecosystem, and improving soil water conservation capacity is the key to enhance the water holding capacity of vegetation system.
2023 Vol. 21 (1): 19-28 [Abstract] ( 274 ) [HTML 1KB] [PDF 3356KB] ( 114 )
29 HUANG Jiahui, LIU Yuanqiu, XU Qing, LI Lehuan, WEN Linsheng, ZHENG Xiling, LIU Chunmei, DENG Wenping
Time lag effects of throughfall on the canopy of Cryptomeria japonica in Lushan Mountain, China under different rainfall intensity
[Background] The redistribution of precipitation by forest has always been a hot spot and difficulty in hydrology research. Japanese cedar (Cryptomoria japonica) is the main afforestation tree species in Lushan Mountain, which plays an important role in ecological function such as soil and water conservation, atmospheric purification, and forest recreation. The purpose of this article is to explore the penetration rain process under different rainfall characteristics.[Methods] We did a research on monitoring data of real-time rainfall process of C. japonica forest in Lushan Natural Protection Area from April 2017 to September 2017 based on Lushan Ecosystem Observation and Research Station. And then we selected part of typical rainfall events (three different rainfall levels), and analyzed time lag effects in different rainfall intensity. Through the 5-point method, the throughfall sample points were arranged on sample plot in forest, rainfall sample points were arranged on outside forest, and the data for both of them were collected through the auto rain gauge.[Results] In the rainy season of 2017, the rainfall characteristics of the Lushan Mountain were low (≤ 5 mm), low rainfall intensity(≤ 2 mm/h) and short duration of rainfall(≤ 2 h). During initial lag time from the beginning of rainfall outside the forest to the beginning of rainfall inside the forest, the initial lag time y decreased rapidly with the increase of the rainfall intensity x outside the forest, showing a power function relationship (y=0.656x-0.822, R2=0.823 4). The relationship between the initial lag time and the rainfall outside the forest was not obvious. The statistical results showed that the average rainfall intensity with positive canopy retention effect was smaller than that with the negative retention effect, and the most retention effect at ≤ 2 h and >8 h of rainfall duration was positive, and negative retention effect was evident at >4~8 h of rainfall reaching peak (mid rainfall duration).[Conclusions] The characteristics of rainfall (rainfall intensity and duration) determine the process of throughfall, and then affect time lag effects of canopy. It can be found that in the process of rainfall, the effective time lag effects of canopy on rainfall mainly occur in the beginning and end of rainfall, while in the middle rainfall duration, the effect of canopy interception can almost be considered to be ignored, and the rainfall intensity inside the forest is greater than that outside the forest.
2023 Vol. 21 (1): 29-36 [Abstract] ( 267 ) [HTML 1KB] [PDF 1450KB] ( 115 )
37 CHEN Yuxin, ZHENG Bofu, FU He, LUO Chengkang, JIANG Yihui, ZHU Jinqi
Effects of roots in different vegetation types on soil water distribution
[Background] As one of the ecological disasters in the world, shallow landslides are closely related to the distribution of water in soil. Therefore, a good water distribution pattern in the soil is helpful to improving the ecological risk resistance. In this paper, the effects of roots of different vegetation types on soil water distribution were analyzed.[Methods] Taking the typical coniferous and broadleaved mixed forest, Phyllostachy sheterocycla forest and fallow land in Wuning county in the north of Jiangxi province as research objects, the soil water distribution was observed by staining tracer experiment. Soil and root samples were collected to determine the soil physical and chemical properties, plant root characteristics, soil water storage capacity, stability of soil aggregatesand other indicatorsof 0-20 cm, 20-40 cm, and 4060 cm soil layers, respectively. Combined with stainingcondition, the multiple effects of root and soil characteristic indexes on soil water distribution were analyzed.[Results] 1) Both coniferous and broadleaved mixed forest and P. heterocycla forest showed large area staining in 0-60 cm soil layer, but only in 0-20 cm soil layer in fallow land. The more the soil layer of the root system, the more prominent the stained area. 2) Soil water content, maximum water-holding capacity, saturatedmoisture content, mean weight diameter and geometric mean diameter decreased significantly with the increase of soil depth. 3) The number of roots in coniferous and broadleaved mixed forest and P. heterocycla forest was 16.96 times and 30.95 times as much as that in fallow land, respectively (P<0.05). The water storage capacity (maximum water-holding capacity) of the deep layer (40-60 cm) was 3% and 10% higher than that in fallow land, respectively, and the soil aggregate stability (mean weight diameter) was 13% and 23% higher than that in fallow land, respectively. 4) Root characteristic index, soil water storage capacity index and soil aggregate stability index were positively correlated with dyeing area ratio (P<0.05).[Conculsions] In the three types of experimental plots, the rich roots in the soil obviously promote the soil water storage capacity and the stability of soil aggregates, and further promote the water distribution in the soil, thusthe water distribution of coniferous and broadleaved mixed forest and P. heterocycla forest is stronger than that of fallow land.In order to effectively improve the function of regional soil and water conservation and ecological risk resistance, it is necessary to strengthen the management and protection of forest resources and improve the diversity of woodland vegetation so as to increase the distribution density and depth of underground roots.
2023 Vol. 21 (1): 37-46 [Abstract] ( 341 ) [HTML 1KB] [PDF 9165KB] ( 157 )
47 LIU Yuansheng, CHEN Zuyong, LIU Fang, ZHU Jian, BU Tongda
Effects of naturally-restored vegetation on the available nutrients and microbial community diversity of coal gangue matrix
[Background] The ecological environment management in most closed small coal mines in central and western Guizhou had achieved obvious results. The natural growth of Pinus massoniana, Betula luminifera, and Neyraudia, plant communities had appeared in coal gangue dumps piled in the open air for many years. Discussing the change and correlation of the nutrient and microbial community diversity of coal gangue matrix under the different types of natural vegetation are of great significance.[Methods] A sample plot (20 m×10 m) was set up in the coal gangue yard, we investigated 3 types of vegetation (Pinus massoniana young forest,Betula luminifera+Castanea seguinii young forest, and Neyraudia grass) and collected their dominant plants recovered from coal gangue dumps in the closed coal mine area in central Guizhou, and collected the coal gangue matrix samples from 3 types of vegetation or the rhizosphere of dominant plants at the same time. Moreover, the available nutrient content of coal gangue matrix was determined by conventional analytical methods and the functional diversity analysis of microbial communities was performed using the ECO MicroPlate of BIOLOGTM.[Results] 1) In the process of natural vegetation restoration, the organic carbon(C) and the effective nitrogen (N) contents of the coal gangue matrix increased significantly, and the effective phosphorus (P) and potassium (K) contents also increased to varying degrees, and the order of their effects was B. luminifera+C. sequinii young forest >P. massoniana young forest >Neyraudia grass and there were significant differences in available N contents of coal gangue matrix among the three vegetation types, and the organic C and available N contents of coal gangue matrix under B. luminifera+ C. sequinii young forest or P. massoniana young forest was significantly higher than those of Neyraudia grass. Also, the order of contents of organic C and available N, P and K in the coal gangue matrix of the dominant plant root zone was B. luminifera>Neyraudia>P. massoniana. 2) After the natural restoration of vegetation, the microbial community richness index H and dominance index D of the coal gangue matrix were significantly higher than those of the bare coal gangue matrix, especially B. luminifera+ C. sequinii young forest. The microbial community H of coal gangue matrix under different vegetation types had a significantly positive correlation with the contents of organic matter C, available N, effective P and effective K. However, the microbial community D and available N contents were extremely significantly positively correlated.[Conclusions] In the process of natural vegetation restoration, the organic C and available N, P and K mass fractions and microbial community diversity of coal gangue matrix increased significantly, especially in the young forest of B. luminifera+ C. sequinii.
2023 Vol. 21 (1): 47-54 [Abstract] ( 284 ) [HTML 1KB] [PDF 840KB] ( 127 )
 
Applied Studies
55 CHENG Yuzhuo, ZHAO Wenting, JIAO Juying, ZHANG Liping, CAO Xue, CHEN Tongde, LI Jianjun, ZHANG Ziqi
Soil conservation effect of cropland use change in the Yellow River-Huangshui River Valley over the past 20 years
[Background]Soil conservation is a regulatory service provided by ecosystems to reduce soil erosion. By altering the surface environment,soil conservation function has been greatly affected by human land use activities in recent years.Yellow River-Huangshui River Valley (YHV), the main agricultural area of Qinghai province, has had huge changes in the use of croplandand soil conservation under the dual drive of the project of returning farmland to forests and the large-scale development of the western region in the past two decades. The analysis of its soil conservation function and its dynamic soil conservation effect may provide a scientific basis for local land spatial planning and soil and water conservation program design and policy management.[Methods]In this study, cropland, abandoned cropland, and converted forestland from 2000 to 2010 and 2000 to 2018 in the YHV was extracted using supervised classification and normalized difference vegetation index (NDVI) time series changes. Then,by using rainfall datasets, soil property, digital elevation model (DEM), annual maximum NDVI and land use datasets, the soil conservation in YHV from 2000 to 2018 was simulated and the soil conservation effect of cropland change was analyzed based on Universal Soil Loss Equation (USLE).[Results]1) From 2000 to 2018, the land use change in the YHV was mainlythe decrease of cropland (6.08%), the increase of construction land and forest(1.45% and 8.06%).The loss of cropland was principally transferred to grassland, forest and construction land, which were mostly distributed in Qianshan area, the edge of Naoshan areas and river valleys, indicating that the change of cropland in the YHV in recent years was greatly affected by the project of converting cropland to forest and urbanization.2) In the past 20 years, the amount of soil conservation has continued to increase.Forest and grassland had accounted for more than 84% of the total soil conservation in the study area.The transfer of cropland to grassland and cropland to forest both resulted in soil conservation benefits, and the later had higher value because it mostly distributed in the Naoshan area with better water resources.Moreover, the soil conservation benefit of the cropland transfer in the Naoshan area was better than that in the Qianshan area, while the soil conservation amount of the cropland transfer plots in the flat terrain area such as river valley and loess tableland was even lower than that of the cropland in the same area.[Conclusions]Using RS technology and USLE model, the distribution and change characteristics of land use and soil conservation in the YHV from 2000 to 2018 were quantitatively assessed. In the YHV, the soil conservation effect of cropland change is obvious, and it is greatly affected by terrain and water resources.It will be the direction of soil and water conservation management in the future to adjust the structure of cropland and abandoned cropland and ensure the stable and long-term providing of vegetation and soil conservation function.
2023 Vol. 21 (1): 55-63 [Abstract] ( 305 ) [HTML 1KB] [PDF 4473KB] ( 146 )
64 LI Zhiguang, WANG Junxiong, WANG Haiyan
Index system for evaluating the carbon sink capacity of regional soil and water conservation
[Background] Scientific and systematic evaluation index system of soil and water conservation carbon sink capacity can provide basic data for quantitative analysis of soil and water conservation carbon sink capacity in a region, which is of great significance for guiding the implementation of soil erosion control measures, and providing information of soil and water conservation for the realization of carbon neutralization goals in China.[Methods] Based on the mechanism, pathways and material performances of soil and water conservation carbon sink, referred to the carbon sink evaluation methods of terrestrial ecosystem, and combined with the basic data of soil and water conservation measures and their benefits, the technical route "soil and water conservation measures and their benefits (carbon sink material basis) → carbon sink pathways → material performances of carbon sink → carbon sink quantity"was proposed and adopted to analyze and clarify the evaluation index system of soil and water conservation carbon sink capacity.[Results] The index system includes 5 primary and 11 secondarysoil and water conservation measures and their benefit indexes, as well as the corresponding carbon sink rate and organic matter content, such as soil and water conservation forest land, grassland, basic farmland, water retaining body and their benefits.[Conculsions] The evaluation indexes of regional soil and water conservation carbon sink capacity proposed in this study areused to monitor, estimate and count the carbon sink function size of regional soil and water loss prevention and control measures and their benefits. On the regional spatial scale, they have the operability of synchronous implementation with statistical work and convenient data acquisition. In the dimension of estimation parameters, they have the spatial correspondence and accuracy between the location and number of observation points and the estimation results. The evaluation results can be used for analyzing of regional carbon sink capacity and its change trend, for evaluating of ecosystem quality and protection effectiveness.
2023 Vol. 21 (1): 64-72 [Abstract] ( 336 ) [HTML 1KB] [PDF 834KB] ( 326 )
73 DAI Yuquan, XIAO Li, LIU Wenhu, LIU Yanmei, ZHANG Qian, HUANG Chengmin
Benefit evaluation of runoff and sediment reduction measures on the earth slopes in mountainous areas, Southwest China
[Background] In view of high and steep slope with frequent heavy rainfall, the measures against extreme soil erosion have been taken commonly on the cut-slope in mountainous areas. However, the characteristics, process and influencing factors of soil erosion on the earth cut-slope with or without soil and water conservation measures are rarely reported. The earth cut-slopes in four mountainous regions of Sichuan and Yunnan provinces, Southwest China were selected to evaluate the benefit of runoff and sediment reduction resulted from soil and water conservation measures under multiple rainfall intensity, and examine the effect of soil compactness on sediment yield.[Methods] Here, the effects of nine measures, i.e., bare slopes, step rills, gravel, three-dimensional (3D) network, vegetation plus 3D network, different vegetation coverage (25%, 50%, 75% and 90%) against soil erosion on runoff and sediment reduction as well as the relationship between surface soil compactness and sediment yield have been executed on forty-five road cut-slopes at 12 sites in Panlong and Qiling counties of Yunnan province and Wenchuan and Songpan counties of Sichuan province, southwestern China, by setting up micro-runoff plots with simulated rainfall. The surface runoff and sediment yields produced in 45 earth slopes under various measures were determined by runoff plots with an area of 2 m2. The soil pH, organic matter content, particle and aggregate size distribution on each earth slope also were analyzed.[Results] The tested slope soils generally have coarser texture relative to undisturbed slope soils, and are dominated with the particle size fraction of sand and silt, occupying an averaged range of 36.9% to 54.1%, and 18.3% to 50.4%, respectively. Structural failure rate of the soil aggregates varies greatly from 20.8% to 63.3%, indicating the erosion durability of soils with the highest rate in Songpan is relatively low. Except the treatment that the surface soil covered with gravels, the runoff and sediment yields on slopes with protection measures are significantly lower than those on bare slope, with the runoff and sediment yields of higher than 1 700 mL and 100 g, respectively. Among them, the measures, i.e., vegetation plus 3D network and vegetation with the coverage more than 75%, are the most effective in mitigating runoff and sediment yields. With the increase of vegetation coverage from 0 to 90%, in general, runoff and sediment yields on cut-slopes significantly declined. The compacted degree values of the bare soil within a depth from the surface to 10 cm on the earth cut-slope varied greatly, fluctuating between 400 and 2 000 kPa. After rainfall, the average compactness of the soil within a depth from the surface to 10 cm dropped by 4 to 373 kPa. The variation of soil compactness would cause the changes in porosity, grain cohesion, and other mechanical properties of soils. In case the soil compactness exceeds 200 kPa, sediment yields on the bare slope would reduce as the soil compactness increases.[Conclusions] The measure with the vegetation coverage more than 75% is the most effective in mitigating runoff and sediment yields, while the nonlinear relationship between soil compaction and sediment yield on bare slope is found.
2023 Vol. 21 (1): 73-82 [Abstract] ( 342 ) [HTML 1KB] [PDF 4271KB] ( 158 )
83 LI Fan, WANG Jiongqi, LIU Zigang, ZHAO Haichao, HE Jiangpeng, HUANG Zhihong, LU Haibo
Effects of land use types on the phosphorus component of soil aggregates and phosphorus pool management index
[Background]The Bashang region in the Northwest Hebei is an important water source in Beijing-Tianjin-Hebei. The soil and water conservation capacity of this region is greatly affected by land use types. This work is to explore the stability mechanism of soil aggregate structure on phosphorus under different land use types.[Methods] Soil samples from 7 land use types, i.e., potato field, oat field, silage corn field, open vegetable field, grassland, woodland and greenhouse vegetable field were collected. Then the soil aggregates were classified by dry sieving method to analyze the distribution law of phosphorus forms and the change of phosphorus pool management index (PPMI) in different soil aggregates. The result data were processes by Excel 2007 and SPSS 20.[Results] The content of total phosphorus (TP) in Northwest Hebei ranged from 211.72 to 441.94 mg/kg, mainly distributed in the aggregates of ≥ 0.25-0.50 mm, and water-soluble total phosphorus (WSTP) content ranged from 267.68-421.83 mg/kg, mainly distributed in the aggregates of ≥ 1.00-2.00 mm. The phosphorus pool management index (PPMI) of soil aggregates ranged from 79 to 153, with the highest value of 0.50 to 1.00 mm aggregates. The contents of water-soluble phosphorus of ≥ 0.25-0.50 mm, the TP content and proportion of ≥ 0.50-1.00 mm, and the PPMI of <0.25 mm increased in the potato field. The oat field promoted the distribution of phosphorus to the aggregate of ≥ 5.00 mm and increased PPMI. The distribution of soil TP to ≥ 1.00-2.00 mm aggregate were promoted, and the PPMI of the ≥ 0.50-1.00 mm soil aggregates increased in the silage corn field and forest land. The management index of aggregate phosphorus pool ≥ 0.50-1.00 mm was improved in the grassland. The TP content and proportion of aggregates ≥ 5.00 mm in the vegetable field, the PPMI of <0.25 mm in the greenhouse vegetable field, and the PPMI of ≥ 0.50-1.00 mm aggregate increased in the open vegetable field.[Conclusions] Large soil aggregates can increase the supply capacity of soil phosphorus holding capacity. Therefore, in the Bashang region of Northwest Hebei, the methods of adding organic fertilizer, rotating crops with high return rate, controlling potato planting, and increasing forage grass planting should be used to promote the distribution of phosphorus to the big aggregate and deduce the loss of phosphorus, thus improving the ecological benefits of the Beijing-Tianjin-Hebei water source area.
2023 Vol. 21 (1): 83-91 [Abstract] ( 297 ) [HTML 1KB] [PDF 1104KB] ( 125 )
92 ZHANG Liwen, WANG Xiuru, SONG Liqiao, LI Rui, SHU Guobiao, BAI Xuexin
Evaluation of hydrological situation in Guanhe Basin, a tributary of Jinsha River
[Background] The Jinsha River is the main sand-producing area in the upper reaches of the Yangtze River. Studying the characteristics and driving factors of water-sediment changes in the Jinsha River is of great significance to the implementation of soil and water conservation measures in the future, the regulation of the relationship between water and sand in the Yangtze River, and the rational use of water resources.[Methods]This paper selects the water and sediment data of the Doushaguan Hydrological Station from 1959 to 2018 for a total of 60 years, and uses the Mann-Kendall trend analysis and the hydrological index change range method (IHA/RVA) to determine the annual runoff and annual sediment transport. The double cumulative curve method and the cumulative slope rate of change method were used to quantitatively calculate the impact of human activities on the water and sand regime.[Results] 1) The multi-year average discharge and total annual precipitation at Doushaguan Hydrological Station from 1959 to 2018 showed a downward trend, but the trend was not significant; the annual average sediment transport rate showed a downward trend, with a significant trend. 2) After soil erosion control, the hydrological change degree of the monthly average discharge value of Doushaguan Station Hydrological Station reached 34%, showing a moderate change; the hydrological change degree of the monthly average sediment content value reached 40.58%, showing a moderate change. 3) Human activities, annual precipitation, and annual potential evaporation contribute 69.22%, 29.66%, and 1.12% to the annual sediment transport, respectively. The total sediment reduction affected by human activities is 2 564.66×104 t, and average annual amount was 116.57×104 t Human activities were the most important factor influencing changes in sediment transport of Guanhe Basin.[Conclusions] This paper analyzes the change trend of water and sediment before and after the impact of human activities in 1996, and the degree of change in the hydrological indicators of the Guanhe Basin for a total of 60 years in the two phases, and further explores the changes in water and sediment regimes before and after soil erosion control. Provide reference for ecological protection and restoration of Guanhe River.
2023 Vol. 21 (1): 92-100 [Abstract] ( 299 ) [HTML 1KB] [PDF 1995KB] ( 140 )
101 HU Ke, HAN Nianlong, YU Miao, ZHANG Yucheng
Land use change simulation in Sanya city based on remote sensing ecological index
[Background] With the continuous promotion of urbanization in China, the contradiction between ecological protection and economic development is becoming increasingly prominent. Strengthening the monitoring and rigid constraints of the ecological environment in the process of urban development is conducive to ecological environmental protection and provides a carrying capacity base for sustainable economic and social development. Sanya is a typical city in the tropical region of China and has faced many ecological and environmental problems in the rapid expansion of the city in recent years. Therefore, there is an urgent need to conduct quantitative spatial assessment and scenario simulation studies on the ecological environment of Sanya city by establishing a research framework for land use change and ecological environment monitoring.[Methods] This study assessed and monitored the ecological quality of Sanya city based on Landsat remote sensing images in 2014 and 2018, using the Remote Sensing Ecological Index (RSEI) formed by integrating four ecological elements of greenness, humidity, heat and dryness by principal component analysis. The RSEI monitoring results were classified into different ecological constraints according to ecological quality levels, and combined with the PLUS model to simulate land use changes in Sanya city in 2030 under three scenarios of natural development, moderate ecological constraints and strict ecological constraints.[Results] The RSEI of Sanya city decreased from 0.656 to 0.632 between 2014 and 2018. Although the greenness, humidity increasing and heat decreasing improved the ecological environment, but the increasing in dryness contributed more to ecological damage than the first three, resulting in a decrease in the overall RSEI in Sanya city. From 2014 to 2018, the area of RSEI with excellent ecological quality decreased by 132.19 km2 and the area of RSEI with poor ecological quality increased by 14.48 km2. As a result, the overall ecological quality of Sanya city has deteriorated and ecological degradation occurred mainly in the hot spots of the city's economic development. Based on the PLUS model to simulate land use changes in Sanya city in 2030, the results showed that under the natural development scenario, construction land expanded significantly, mainly by encroaching on woodland and arable land, with the total reduction of woodland being the largest, indicating that this scenario posed a threat to ecological and arable land security. The simulation results of the two ecological constraints scenarios combined with RSEI showed that the expansion of construction land and the decline of woodland were both controlled, and the strict ecological constraints scenario had a more obvious effect on the protection of ecological space.[Conculsions] The study shows that RSEI-based can achieve rapid and effective monitoring of the regional ecological environment. According to the scenario simulation combining ecological constraints, it is shown that strengthening ecological constraints can effectively reduce the significant expansion of construction land and the maintenance of forest quantity. This study may provide reference cases for the implementation of land use planning and sustainable development under ecological constraints in tropical cities.
2023 Vol. 21 (1): 101-109 [Abstract] ( 265 ) [HTML 1KB] [PDF 3887KB] ( 128 )
110 JIN Feng, GE Wenyan, QIN Wei, HAN Jianqiao, MA Tao, ZHENG An
Spatiotemporal variation of vegetation and its future development potential in Gansu province
[Background]Being an important part of terrestrial ecosystem, vegetation plays a crucial role in soil maintenance, climate regulation and carbon sequestration. As a typical climate-sensitive and ecologically fragile region, Gansu province is inseparable from vegetation for soil and water conservation and ecological restoration. Therefore, large-scaled soil and water conservation projects and ecological projects have been implemented to restore vegetation and improve ecological environment at the end of the last century and the beginning of this century. This study is aimed to explore the effectiveness of afforestation and the restoration potential of future vegetation in Gansu province.[Methods] The linear regression method and sliding-window similar habitat potential model (SWSHPM) were applied to analyze the spatiotemporal variations of vegetation and its future restoration potential, using MODIS (moderate resolution imaging spectroradiometer) EVI (enhanced vegetation index) data of the growing season (April-September) from 2000 to 2020 and the land use and land cover (LULC) data of 2020.[Results] 1) Generally, EVI increased significantly during the growing season from 2000 to 2020 across the study area, with an average annual growth rate of 0.002/a. The growth rate slowed down from 2012 to 2016 and then speeded up again, indicating the continuous improvement of the overall vegetation coverage in Gansu province during the past 20 years. 2) In terms of spatial variation, EVI decreased from the southeast to the northwest during the growing season in Gansu province, with average annual slopes of -0.006-0.010/a. Besides, the vegetation coverage demonstrated significant and rapid increases in about one-third of the study region, dominated by Longdong and Longnan areas. 3) Longnan and Hexi were the high value and low value areas of EVI, respectively. And the increase of the latter vegetation was the weakest. In addition, spatial variations of EVI in Longzhong and Longdong were relatively small. 4) The vegetation restoration potential index (VRPI) in Gansu province achieved remarkable results. The current vegetation restoration potential achieved degree (VRPAD) was relatively high. The surplus vegetation restoration potential degree (SVRPD) was relatively low. Specifically, 47.4% of the bare land has the potential to be transformed into grassland and forest land. Additionally, 28.1% of grassland area and 2.5% of woodland area had the potential to be improved in the future, respectively.[Conclusions] Overall, the vegetation coverage in Gansu province has improved significantly from 2000 to 2020, while its characteristics of spatial heterogeneity remained unchanged. Besides, there were only about 10% in vegetation coverage for improvement in the future after removing the unnatural vegetation in the study area.
2023 Vol. 21 (1): 110-118 [Abstract] ( 334 ) [HTML 1KB] [PDF 5641KB] ( 157 )
 
Development Studies
119 YU Enxu, ZHANG Mingfang, XU Yali, SUN Pengsen, MENG Zuozhu
Development and application of a regional forest water conservation function assessment tool
[Background] Multiple types of forest changes including deforestation, insect infestation, fire, and afforestation coupled with forest growth and restoration occur at a regional scale, which lead to the restoration effects of forest and associated water conservation capacity accumulate over space and time. The Zagunao watershed has suffered from deforestation in the past decades, which has severely reduced its water conservation capacity. This paper focuses on the forest change dynamics and the corresponding restoration of the water conservation capacity in this watershed under a series of ecological protection projects. However, traditional assessment tools of forest water conservation function lack the description of the spatial-temporal cumulation of forest growth and associated water conservation capacity, and are featured with complex computation, which impedes the evaluation on the effects of forest restoration on water conservation in a rapid and accurate way.[Methods] To address this issue, we innovatively developed the Equivalent Recovery Area (ERA) model for describing the hydrological function recovery with forest changes after forest deforestation and assessing the spatial-temporal dynamics of cumulative forest recovery after forest logging. Then, through combining the forest restoration evaluation model (ERA) and classic forest water storage function evaluation method (comprehensive water storage capacity method), this study took advantage of ENVI/IDL, ArcGIS Engine/C#.Net GIS to develop a GIS-based tool for assessing regional forest changes and associated forest water conservation function dynamics. The tool named Regional Forest Water Conservation Function Assessment Model (RFWCFAM) supports to evaluate the spatial-temporal changes of forest landscapes and forest water conservation functions under natural and artificial recovery scenarios. Charts and spatial distribution maps of forest changes, water conservation capacity dynamics, and restoration measures layout generated, after inputting precipitation, vegetation/forest, soil, and forest restoration measures data in RFWCFAM.[Results]This tool was successfully applied in the Zagunao watershed. According to the assessment, the EHFR (equivalent hydrological function recovery) coefficient increased in study area with the implementation of natural and artificial restoration measures from 2010 to 2030. The canopy, litter, soil and total forest water conservation capacity of the Zagunao watershed were about 129.8, 25.96, 523.62, and 697.37 t/hm2, respectively, in 2010, and all layers showed consistent upward tendencies from 2010 to 2030 under both natural restoration and artificial restoration scenarios. The artificial restoration measures yielded better effect on forest water conservation function than natural restoration. By 2030, the forest water conservation capacity of artificial restoration scenario is expected to be about 5.19% higher than that of natural restoration scenario.[Conclusions] The RFWCFAM has addressed the limitations of the traditional water resource assessment method and has been successfully applied and validated in the Zagunao watershed. Additionally, the RFWCFAM can provide an effective assessment tool to forest and water managers for evaluating the potential effects of forest restoration on water conservation function, along with scientific supports for adaptive forest management and soil and water conservation project evaluation and management in restorations of forest ecosystem functions in China.
2023 Vol. 21 (1): 119-127 [Abstract] ( 300 ) [HTML 1KB] [PDF 3969KB] ( 133 )
 
Forum
128 KANG Rui, QIU Xinling, MA Hongcai, SONG Pengyu
Automatic extraction of disturbed patches in production and construction projects based on deep learning
[Background] Rapid acquiring the disturbance range of production and construction projects is critical for improving the efficiency of soil and water conservation supervision and inspection, and for controlling man-made soil erosion. The plots for production and construction projects are numerous and scattered, but remote sensing technology can achieve timely and accurate acquisition of their spatial distribution. At present, the remote sensing interpretation of disturbed patches in production and construction projects is mainly based on human-computer interaction with less automatic extraction. The existing algorithms are highly specialized and low in regional applicability, which makes it difficult applying in engineering.[Methods] The central and eastern parts of Gansu province were used as the research area, and deep learning algorithms were applied to carry out research on automatic extraction of disturbance areas. Based on GF-1 and GF-6 satellite images, the disturbance characteristics of production and construction projects were summarized, and bare land and newly added construction land were determined as the characteristic features detecting in production and construction projects. Selected 1 156 disturbances totally for the patch samples, then the enhanced DeepLabV3+ model and the U-Net model were utilized to construct an automatic extraction model of disturbance patches. Based on automatic extraction, the minimum recognition area was set to reduce the interference of mini patches. The extraction effects of different models and different minimum recognition areas were quantitatively evaluated by indicators such as quantity recall rate, quantity accuracy rate, area recall rate, and area accuracy rate.[Results] 1) The DeepLabV3+ model had fewer erroneous image spots. The quantity accuracy rate was more than 15% than that by the U-Net model, and the area accuracy rate was slightly higher than the U-Net model. 2) In Chengguan district and Zhengning county, the DeepLabV3+ model had fewer missing image spots, and the quantity recall rate was more than 5% higher than that of the U-Net model. The quantity recall rate of the DeepLabV3+ model in Baiyin district was slightly lower than that of the U-Net model. 3) Large patches extraction of these two models was better. The area accuracy rate was higher than the quantity accuracy rate, and the area recall rate was higher than the quantity recall rate. 4) As the minimum recognition area increased, the area accuracy of the model increased and the area recall rate decreased. 5) When the minimum recognition area was 1 hm2, utilizing the DeepLabV3+ model generated the best extraction effect. The average quantity accuracy rate was 78.31%, the quantity recall rate was 61.69%, the area accuracy rate was 88.82%, and the area recall rate was 80.60%.[Conclusions] In summary, DeepLabV3+ model has better overall classification effect. After setting an appropriate minimum recognition area, it can balance the accuracy and recall of the automatic extraction results. At the same time, the model has good extraction results in different districts and counties, which indicates that the deep learning algorithm has strong regional applicability and can be applied to a wide range of remote sensing supervision work.
2023 Vol. 21 (1): 128-138 [Abstract] ( 292 ) [HTML 1KB] [PDF 10320KB] ( 183 )
139 ZHANG Li, LIU Jiayu
Ecosystem service dynamics in sandy land in Northeast China during the past 30 years
[Background] The sandy land in Northeast China (Horqin sandy land, Songnen sandy land and Hulunbuir sandy land) belongs to the transition zone from semi-arid and semi-humid area to semi-arid area. The desertification of sandy land is serious, thus it is urgent to carry out ecosystem services. Revealing the temporal and spatial evolution characteristics of ecosystem services in this region over a long period of time may provide a scientific basis for ecological restoration and soil and water conservation in sandy land.[Methods] Based on the InVEST model and using data such as land use data, vegetation cover, digital elevation models, soil quality, etc., the article evaluated the functions of soil conservation, water conservation, carbon storage and habitat quality of this area from 1990 to 2020.[Results] 1) The total amount of soil conservation in sandy land of Northeast China increased by 1.98×107 t/a, and the high-value areas were concentrated in the southwest of Horqin sandy land, the east and west of Songnen sandy land, and the east of Hulunbuir sandy land. 2) The water conservation showed an overall increasing trend with an increase rate of 2.88×107 mm/a. The high-value areas were concentrated in the southeast of Horqin sandy land, the northeast of Songnen sandy land and the east of Hulunbuir sandy land. 3) The carbon storage increased by 1.60×106 t/a. The high-value areas were mainly distributed in the northeast of Horqin sandy land, the east and west of Songnen sandy land and the east of Hulunbuir sandy land. 4) The average habitat quality index changed little overall and it showed a trend of first increasing and then decreasing, the high-value areas were concentrated in the east and west of Songnen sandy land and the east of Hulunbuir sandy land.[Conculsions] The four major ecosystem service functions of soil conservation, water conservation, carbon storage and habitat quality in sandy land in Northeast China showed an overall increasing trend, and the increasing areas showed a certain spatial aggregation. From 1990 to 2020, the land use types of sandy land in Northeast China were mainly cultivated land, grassland and forest land. The area of cultivated land, construction land, sandy land and other unused land is on the increasing trend, while the area of forest land, grassland and water area is on the decreasing trend. This form of land use change has important implications for the spatiotemporal evolution of ecosystem services.
2023 Vol. 21 (1): 139-148 [Abstract] ( 228 ) [HTML 1KB] [PDF 5936KB] ( 134 )
中国水土保持科学
 
Notice on the Recruitment of Youth Editorial Board Members for the Journal of SSWC
Theme on Spreading Spirits of Great Scientists: LIANG Xi, the Founder of Forestry Education in China
ZHENG Fenli, CHEN Liding and LEI Tingwu in the list of Highly Cited Chinese Researchers by Elsevier
SSWC Indexed in the 2020 edition of “A Guide to the Core Journals of China”
Science of Soil and Water Conservation Accepted for Inclusion in Scopus
2020 Editor-in-Chief Meeting of Science of Soil and Water Conservation Held in Beijing, Concurrently
SSWC Selected to Be in Core Library of Source Journals of CSCD during 2019-2020
SSWC Indexed in the 2017 edition of “A Guide to the Core Journals of China”
Appreciation for peer reviewer of SSWC Editorial Board
2017 Editor-in-Chief Meeting of Science of Soil and Water Conservation Held in the Yangling of Shaan
Professor Wang Lixian, Former Editor-in-Chief of SSWC Won Norman Hudson Memory Award
Calls for Papers in English
Deputy Editor-in-Chief Cui Peng Elected as a Member of 9th National Committee of CAST
Three Members of SSWC Editorial Board Rewarded as NOSTW in 7th Session Assessment
Election of 4th Editorial Board and First Meeting of New Board Held in Beijing
Deputy Editor-in-Chief of SSWC, Academician Cui Peng elected as a member of the IRDR SC
Notice About The 5 Not-Allowed Rules While Publishing Academic Articles by 7 Organizations
SSWC Indexed in “A Guide to the Core Journals of China”
Science of Soil and Water Conservation Calls for Papers
SSWC Selected to Be in Core Library of Source Journals of Chinese Science Citation Database During
On the Home Page of the Journal Science of Soil and Water Conservation
Five Papers of Science of Soil and Water Conservation Determined as Excellent in 5th Assessment
Congratulations to Deputy Editor-in-Chief Cui Peng Elected as Academician of Chinese Academy of Scie
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