中国水土保持科学
中国水土保持科学
 
 
 
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2023 Vol.21 No.4  Published 2023-08-30
  
 
Foundamental Studies
1 FENG Ziqi, SUN Wenyi, MU Xingmin, GAO Peng, ZHAO Guangju
Effects of vegetation restoration methods on soil moisture in the small basins of Loess Plateau gully region
[Background] Large-scale vegetation restoration, especially afforestation, has intensified the evapotranspiration process, the deep soil of the Loess Plateau has dried up, and the runoff of the Yellow River has been reduced, and vegetation restoration has approached the threshold of water resources and vegetation carrying capacity. Vegetation restoration may significantly improve soil structure, increase soil water infiltration, and improve soil water holding and storage capacity, which in turn affects changes in basin yield, confluence, and sediment transport. This is of great significance in studying the soil moisture characteristics of natural vegetation restoration and artificial afforestation under specific climatic conditions for soil and water conservation.[Methods] Based on the comparison of soil physical and chemical properties and continuous high-resolution water dynamic monitoring, analysis of the water holding capacity and storage capacity of the soil in the Dongzhuanggou(DZG) small basin under natural restoration and the Yangjiagou (YJG) small basin under artificial afforestation.[Results] 1) When comparing the DZG small basin with natural vegetation restoration, the soil bulk density and soil porosity of 0-100 cm in the YJG small basin under artificial afforestation and vegetation restorations was 91.9% and 1.1 times that of DZG, respectively. The organic matter content and cation exchange capacity were 21.4% and 22.6% higher than those of DZG, respectively. There was no difference in the physicochemical properties of the topsoil, and the effects of different vegetation restoration methods on the water holding capacity were more profound. 2) Under the same rainfall conditions, the soil moisture content of the DZG 0-80 cm soil layer increased by 8.85% on average, and the total water storage increased by 71.7 mm. YJG 0-80 cm increased by 12.74% on average, and the total water storage increased by 102.1 mm. 3) DZG's soil moisture content responds quickly to rainfall events, while YJG's soil moisture content lags behind the soil depth.[Conclusions] After more than 60 years of vegetation restoration at the Xifeng Soil and Water Conservation Test Station in the Loess Plateau and gully region, the soil water-holding capacity of YJG small basin with artificial afforestation is better than that of DZG small basin with natural vegetation restoration.
2023 Vol. 21 (4): 1-10 [Abstract] ( 186 ) [HTML 1KB] [PDF 2920KB] ( 321 )
11 WANG Litao, XIAO Huijie, XIN Zhiming, JIA Xiaoxiao, YANG Yuli
Numerical simulation of wind speed field in the typical farmland shelterbelts in the oases of the Ulan Buh Desert
[Background] The structural configuration of shelterbelt is crucial to the protective effect of shelterbelt. In the current research on the windbreak effect of farmland shelterbelt, field wind speed observations are mostly used, which is complicated and laborious to measure, and the differences in the windbreak effects of different configurations of shelterbelts are not studied enough. Based on the numerical simulation of the wind speed field of the shelterbelt, this study analyzed the windbreak effect of different configurations of shelterbelts and the distribution characteristics of the wind speed field around the shelterbelt.[Methods] Four different configurations of shelterbelts (0.8H width shelterbelt, 0.2H width shelterbelt, the arbor-shrub mixed shelterbelt and shrub-free shelterbelt, H represents shelterbelt height) in the Ulan Buh Desert were used as study objects. The two-dimensional numerical simulation method was used to simulate the wind speed field around the shelterbelt, and verified with the wind speed measured in the field. The influence of different shelterbelt structures on the characteristics of the wind speed field around the shelterbelt, the horizontal wind speed at different heights, and the efficient protection distance of the shelterbelt was explored.[Results] 1) When the airflow passed through four shelterbelts with different structures and configurations, different speed zones were produced around them, which were respectively the speed lifting zone above the shelterbelt, the weak wind zone behind the shelterbelt, the lower airflow acceleration zone, the reflux zone and the airflow recovery zone behind the shelterbelt. The airflow acceleration zone and the reflux zone were greatly affected by the structure of the shelterbelt.2) The impact on airflow under different shelterbelt widths mainly occured behind the shelterbelt.At a height of 0.1H near the ground, compared with the 0.2H width shelterbelt, the wind speed decreased by 90.8% within 1H behind the shelterbelt and the reflux intensity increased by 55.2% behind the shelterbelt for the 0.8H width shelterbelt, and the efficient protection distance was 17.8H and 15.5H for the two shelterbelts, respectively, which decreased by 2.3H compared with the efficientprotection distance for the 0.2H width shelterbelt. 3) At the height of 0.1H, the wind speed in the arbor-shrub mixed shelterbelt decreased to 0 within 0.7H after the shelterbelt, while the shrub-free shelterbelt showed a significant acceleration of airflow and reached the maximum wind speed at 1H after the shelterbelt, which was about 70.5% of the initial wind speed. Compared with the shrub-free shelterbelt, the wind speed decreased by 122.4% and the reflux intensity increased by 15.9% in the post-shelterbelt 1H range in the arbor-shrub mixed shelterbelt, and the efficient protection distance of the shelterbelt was 21.5H and 23.7H, respectively, which was reduced by 2.2H compared with the shrub-free shelterbelt.[Conclusions] The wider shelterbelt and mixed shelterbelt of trees and shrubs can well improve the wind speed at the back edge of the shelterbelt and effectively suppress the acceleration of airflow near the ground, but also enhance the reflux behind the shelterbelt and shorten the efficient protection distance, so the shelterbelt configuration should be planned reasonably according to different locations.
2023 Vol. 21 (4): 11-19 [Abstract] ( 107 ) [HTML 1KB] [PDF 2245KB] ( 195 )
20 TIAN Xin, ZHAO Yonggang, LIU Qixia, YANG Lu, LIU Xiaofang
Soil saturated hydraulic conductivity and its influencing factors on the slope with long-term plantation of Caragana korshinskii in the loess hilly region
[Background] The saturated hydraulic conductivity (Ks) can characterize the strength of soil water conductivity, which is an important indicator of soil water conductivity and is closely related to eco-hydrology and soil erosion. Artificial shrub planting on slopes is an essential measure for controlling soil and water loss and restoring fragile ecosystems in the loess hilly areas, but the effect on Ks remains unclear. Soil transfer functions are constructed by integrating easily measurable or obtainable soil indices to estimate Ks accurately.[Methods] This study focused on the sloping land planted with Caragana korshinskii for 15, 25, and 35 years and a control wasteland with wild grass in the loess hilly areas of Ningxia. Three random sample plots were set up along the horizontal slope surface, each with three replicates. The characteristics of Ks variation were investigated and its main soil influencing factors at five slope positions, including top-slope, shoulder-slope, up-slope, mid-slope and low-slope were studied, from 0 to 100 cm (0-40 cm with 10 cm intervals, 40-100 cm with 20 cm intervals). Six common soil transfer functions, Cosby1, Cosby2, Weynants, Saxton, Wang, and W sten, were used to fit Ks.[Results] The Ks range was 6.81-60.77 mm/h, and C. korshinskii planting duration and slope position had significant effects (P<0.05). With the increase of C. korshinskii planting years, Ks first increased (15 years of planting) and then decreased in the 0-40 cm soil layer, while Ks continuously increased in the 40-100 cm soil layer. The highest Ks was at the slope bottom, followed by the slope top and middle, and the lowest at the slope shoulder and upper slope. The simulated results of the six selected soil transfer function models indicated that, except for the W sten model considering soil layer depth, the predicted values of other models were all lower than the measured values. Correlation analysis showed that Ks was closely related to other physical and chemical properties except capillary porosity. The influence of soil properties on Ks was mainly closely related to the formation and stability of soil structure. Path analysis identified organic carbon, saturated water content, and bulk density as the key soil factors affecting Ks on the slope, and the constructed soil transfer function model based on these factors can predict Ks changes more accurately.[Conclusions] In summary, long-term C. korshinskii planting on slopes may generally increase Ks, but this change is jointly affected by the sea buckthorn planting duration and slope position. The Ks soil transfer function constructed in this study may provide a reference for simulating and predicting Ks on slopes in the loess hilly areas.
2023 Vol. 21 (4): 20-27 [Abstract] ( 92 ) [HTML 1KB] [PDF 1842KB] ( 203 )
28 LI Yue, LUO Hongfen
Spatio-temporal changes of ecosystem carbon storage in Puding county of central Guizhou province based on InVEST model
[Background] The carbon cycle and greenhouse effect of terrestrial ecosystem have always been the focus of global change research in geoscience, ecology and environmental sciences. Land use change may reflect human land use patterns in an area and plays an important role in spatial soil and water conservation. Regional land use change is the main reason for the change in ecosystem carbon storage, which affects the carbon source and carbon sink effect.[Methods] This paper took Puding county in central Guizhou as the research area, based on the carbon storage and sequestration module of InVEST model and ArcGIS technology, combined with land use data and carbon density data, the carbon storage and its spatial pattern in Puding county of central Guizhou province from 1973 to 2020 were estimated and analyzed. Based on the land use type carbon storage transfer matrix, the influence of land use changes on the spatial and temporal distribution of carbon storage was explored.[Results] 1) The carbon storage of terrestrial ecosystem in Puding county in 1973, 1989, 2003, 2010 and 2020 were 15.868×106 t, 14.196×106 t, 15.022×106 t, 15.834×106 t and 16.529×106 t, respectively, and the carbon storages of ecosystems decreased first and then increased, with an overall trend of increase and a cumulative increase of 661 000 t, indicating that the ecological restoration project in Puding county has achieved remarkable results and the ecosystem service functions had been significantly improved. 2)The spatial distribution showed a significant increase in the northeast and southwest of Puding county, and a significant decrease in the south-central Puding county. The northeast and southwest of the Puding county maintained a stable trend of increasing carbon storage year by year from 1989 to 2020, while the carbon loss in the middle-south of Puding county was significant from 2010 to 2020, and the highest value areas of carbon storage were distributed in the southwest and northeast of Puding county. 3) Dry land, grassland, paddy field and other woodland were converted into shrubland. Dry land, grassland and other woodland into forest land, and the conversion of dry land to paddy field were the main reasons for the increase of carbon storage in the ecosystem of Puding county and sustainable ecological development, indicating that the increase of shrubland, forest land and paddy field in Puding county is beneficial to carbon sink.[Conclusions] The overall carbon reserves of the ecosystem in Puding county have increased, showing the increasing carbon sequestration capacity in the northeast and southwest of Puding county and the decreasing carbon sequestration capacity in the central and southern region of Puding county. In the future, the carbon storage capacity in the south-central Puding county should be emphasized to improve the regional ecosystem quality and soil and water conservation function.
2023 Vol. 21 (4): 28-35 [Abstract] ( 174 ) [HTML 1KB] [PDF 7590KB] ( 190 )
36 DONG Ling, LIU Huiying, TIAN Langyu
Changes and driving factors of runoff and sediment of Tao River watershed in the upper reach of Gan River
[Background] The river system is an important and very active natural system on the earth, and the change of water and sediment is the direct response of the river system to climate change and human activities. The sediment load dramatically decreased at Tao River watershed, the upper Ganjiang River of China, due to natural and human factors. The objective of this study is to quantify the spatial and temporal variation of runoff and sediment load in the typical watershed in upper reaches of Ganjiang River and their potential causes. Better understanding the dynamic of hydrological processes may provide good reference for soil and water conservation, water resources planning and Ganjiang River basin management.[Methods] the Mann-Kendall test and Pettitt test were employed to investigate the temporal trends and abrupt changes of the annual runoff and sediment load at Julongtan gauging station of Tao River watershed from 1958 to 2018. Then the accumulation slope change rates were applied to analyze the relationship of rainfall-sediment during different periods and quantify the drivers of variation of runoff and sediment load.[Results] 1) The average annual precipitation, runoff and sediment transport in Tao River watershed were 1 565.5 mm, 6.036 billion m3 and 1.125 million t respectively. 2) The annual distribution of runoff and sediment was basically stable, mainly concentrated in April-June. 3) There was no significant change trend and abrupt change point in rainfall and runoff in the watershedof 61a, but rainfall and runoff fluctuated significantly in 1972 and 1985. The annual sediment discharge had no significant change trend before the 1990s, but has decreased significantly since the 1990s(α<0.01), and an abrupt change occurred in 2002(P<0.001). 4) According to the relative change point, the whole period was divided into four connected parts of 1958-1972 (stage A), 1973-1985 (stage B), 1986-2002 (stage C), 2003-2018 (stage D).When the period of 1958-1972 (stage A) with weak human activities was taken as a fundamental baseline, the contribution rate of the human intervention to sediment load in stage B, C and D was 79.14%, 92.05% and 100%. As time went on, human activities causeda greater and greater impact on sediment transport in Tao River watershed. 5) The construction of large-scale water conservancy facilities such as reservoirs and large-scale soil and water conservation measures are the driving factors for the reduction of sediment transport in Tao River watershed.[Conclusions] Integrating all these results, this work confirmed clearly that human activities are the main driving factor of variation of runoff and sediment load in the upper reaches of the Ganjiang River basin. The study has important practical significance for accurately evaluating the role of human activities such as hydraulic projects and the sustainable development of watersheds.
2023 Vol. 21 (4): 36-45 [Abstract] ( 77 ) [HTML 1KB] [PDF 1679KB] ( 199 )
46 ZHANG Lu, WEI Jing, SUN Zenghui, FAN Hongjian
Effects of different forest covers on soil properties in an aeolian sandy soil improvement area
[Background] Land desertification has always been a major ecological and environmental problem troubling local people's production and life in the wind-sand and grassy flat area in northern Shaanxi province. How to select trees scientifically after the reasonable mixing of local soft sandstone and aeolian sand soil into soil is still a scientific problem that needs to be further solved. To understand the soil characteristics under different forest cover in the aeolian sand soil remediation area provides the decision basis for tree planting optimization, and has important practical significance for the management and ecological environment restoration of Mu Us Sandy Land.[Methods] In this study, in the soft sandstone remediation project area of aeolian sand soil in Mengjiawan village, Yulin city, Shaanxi province, the forest soil of Caragana korshinskii and sea buckthorn of different years with the same topography, geomorphology and site conditions was selected as the research object, and the natural grassland was taken as the reference. Using the method of time generation and space, topsoil samples (0-20 cm) were collected in 5, 10 and 15 years from the forest lands of the first phase (2007), second phase (2012) and third phase (2017), respectively, to measure the soil density, water content, organic matter and calcium carbonate.[Results] In the aeolian sandy soil area, the soil bulk density and soil calcium carbonate size of different woodlands were as follows:natural barren grassland > C. korshinskii>Hippophae rhamnoides, among which, the soil bulk density of H. rhamnoides was 3.10% lower than that of C. korshinskii, and 10.04% lower than that of the natural barren grassland. The soil calcium carbonate content of the soil was 13.82% lower than that of C. korshinskii, and 37.66% lower than that of barren grassland. The soil moisture content and soil organic matter of different woodlands were as follows:H. rhamnoides > C. korshinskii > natural barren grassland, among which, the soil moisture content of H. rhamnoides was 21.71% higher than that of C. korshinskii, and 96.68% was relatively larger than that of barren grassland. The soil organic matter content of H. rhamnoides was relatively 9.48% were larger than C. korshinskii, and 55.64% were larger than barren grassland. With the increase of planting years after remediation, the soil bulk density and soil organic matter content of different woodlands increased, the soil moisture content was the largest in 10 years of remediation, while the soil calcium carbonate content decreased with the increase of remediation years.[Conclusions] To sum up, through the experimental results of soil characteristics of different forest lands, the problem of tree seed selection after land consolidation in the wind-sand and grass-flat area of northern Shaanxi was solved. The planting of trees has improved the soil structure after the use of feldspathic sandstone to remediate the aeolian sandy soil, among which the planting of H. rhamnoides is suitable.
2023 Vol. 21 (4): 46-52 [Abstract] ( 53 ) [HTML 1KB] [PDF 2127KB] ( 144 )
53 LIU Yunjie, GUO Congcong, YAO Lifang, MA Changming
Characteristics and driving factors of stem diameter change of Ailanthus altissima during the growing season
[Background] The study of the relationship between tree growth and environmental factors is important to improve the water use efficiency of forest trees and the rational management of forest trees. Previous studies have mostly focused on the relationship between tree whorl and climate, which lacks continuity and completeness of observation. A stem radial change recorder can continuously record stem diameter growth and reversible moisture-related shrinkage and swelling within the stem, providing information on the tree's moisture relationships and stem diameter growth.[Methods] The Ailanthus altissima in Hebei was used as the experimental object, and the dynamic variations of stem diameter during the growing season (May 2021 to September 2021) of A. altissima was continuously monitored by means of a radial change recorder, and the sap flow and micrometeorological factors were simultaneously monitored, and the synergistic relationships between stem diameter and sap flow and micrometeorological factors were analyzed by correlation analysis method.[Results] 1) The stem diameter of A.altissima increased by 3 246.856 μm from May to September, and the maximum diurnal variation range presented as June > May > July > August > September, the growth mainly concentrated from early May to mid-July. The diurnal variation of stem diameter showed the regular pattern of periodic contraction and expansion. 2) The variation of stem diameter and sap flow showed a negative correlation (P<0.01), and the variation of stem diameter lagged behind the sap flow for 150, 120, 90, 30, and 30 min from May to September, respectively. 3) The variation of stem diameter also showed a negative correlation with solar radiation, air temperature and vapor pressure deficit, and a positive correlation with air humidity (P<0.01), and there was also time lag. The change in stem diameter lagged behind the change in solar radiation and ahead of the change in vapor pressure deficit. The time lags between stem diameter and each meteorological factor tended to increase as the month progressed. 4) Under the stronger rainfall conditions, the stem diameter of A. altissima increased significantly, and the stem diameter did not shrink back to the original scale afterwards.[Conclusions] The amount of stem diameter growth and variation characteristics varied among different months of the growing season. There is a time lag effect between stem diameter change and sap flow and meteorological factors, and this interrelationship varies in different growth periods. Rainfall is an important factor influencing stem diameter change, and adequate irrigation is beneficial to the radial growth of the stem during the growth stage of the A. altissima in this region.
2023 Vol. 21 (4): 53-59 [Abstract] ( 106 ) [HTML 1KB] [PDF 1706KB] ( 125 )
60 ZHANG Ting, LIU Shiyu, SHENG Fei, WANG Yanyan, YU Minqi, LU Jingyuan
Response of sediment variation to hydrological and meteorological factors in Zhangshui watershed
[Background] Sediment is one of the key hydrological factors in the watershed. In-depth exploration of its variation characteristics and influencing factors is of great significance to the comprehensive management of soil erosion in the watershed. Zhangshui watershed is the main sediment-producing area of Ganjiang river, and it is one of the regions with the longest time series of observation data in Yangtze River basin. In this paper, the Zhangshui watershed in the upper reaches of the Ganjiang river was taken as the study area to analyze the variation characteristics of sediment transport and the direct, indirect and comprehensive effects of hydrological and meteorological factors on sediment transport.[Methods] Based on the measured hydrological and meteorological data from 1961 to 2018, the Mann-Kendall test method was used to analyze the trend change characteristics of sediment discharge, and the wavelet analysis method was used to analyze the periodic change law of sediment discharge. The significant influencing factors of sediment changes were screened by stepwise regression analysis. The direct and indirect path coefficients and decision coefficients of each factor on sediment discharge were calculated by path analysis, and then the direct, indirect and comprehensive effects were analyzed.[Results] 1) The annual distribution of sediment was uneven, showing a single peak distribution, mainly concentrated in April to June; the annual sediment showed an extremely significant decreasing trend (P<0.01). In terms of periodic variation, there were mainly three-fold scales of 3-7, 11-19 and 21-30 years, and the first to fourth main periods of sediment variation were 16, 6, 4 and 25 years. 2) The significant indigenous influencing factors of sediment reduction were runoff, wind speed and temperature, and their contribution rates were 52.5%, 28.8% and -18.7%, respectively. 3) The direct path coefficients of runoff, wind speed and temperature to the reduction of sediment transport were 0.73, 0.40 and -0.26; the direct impacts of runoff, wind speed and temperature on sediment reduction were ranked as follows:runoff > wind speed > temperature. The indirect path coefficients were:-0.03, 0.61 and -0.02; the indirect impacts were ranked as follows:wind speed > runoff > temperature. The decision coefficient was:0.50, 0.14 and 0.17; the comprehensive impacts were ranked as follows:runoff > temperature > wind speed.[Conclusions] Runoff, wind speed and temperature have an important influence on the change of sediment in Zhangshui watershed. The decrease of runoff, the decrease of air temperature and the increase of air temperature are the main reasons for the decrease of sediment in Zhangshui watershed. The research results can lay a theoretical foundation for watershed water and sediment regulation and comprehensive control of soil and water loss.
2023 Vol. 21 (4): 60-68 [Abstract] ( 95 ) [HTML 1KB] [PDF 2808KB] ( 134 )
69 MENG Zekun, WANG Bin, Daniel Moriasi
Effects of the spatio-temporal pattern of single storm on the runoff and sediment yield at watershed scale
[Background] There are many factors affecting the hydrological response at watershed scale. In recent years, more and more studies have been conducted on the effects of spatio-temporal patterns of storm on hydrological response. Most of these studies are based on mathematical models because of the scarcity of high-resolution data. Many research indicated that spatio-temporal patterns of storm events play an important role in runoff discharge and sediment yield at watershed scale. Due to the good data integrity and high resolution, the Fort Cobb watershed in Oklahoma state, USA, was selected as the research site.[Methods] Based on high-resolution meteorological and hydrological data, this study quantified and traced the storm path and spatial distribution of 43 storms in Fort Cobb watershed by using K-means clustering method and Kriging interpolation method. And the effects of storm pattern, rainfall intensity and spatio-temporal characteristics on runoff discharge and sediment yield of Fort Cobb watershed were studied.[Results] 1) The 43 storm events were classified into 4 patterns. Type A, with small rainfall, variable rainfall duration and medium maximum 30-min rainfall intensity. Type B, with small rainfall, variable rainfall duration and small maximum 30-min rainfall intensity. Type C, with medium rainfall, short rainfall duration and medium maximum 30-min rainfall intensity. Type D, with large rainfall, short rainfall duration, and medium maximum 30-min rainfall intensity. Storms with small rainfall and low maximum 30-min rainfall intensity were the commonest pattern. Type C was the main pattern that caused soil erosion in the research area. 2) The runoff discharge and sediment yield were significantly and positively correlated with rainfall and rainfall erosivity (P<0.05) even if under different storm patterns (P<0.05). When the rainfall was the same,different types of storms leads to runoff as C>A>D>B. When the value of rainfall erosivity was equal, different types of storms caused different sediment yield in this area, and the amount from the highest to the lowest was D>B>A>C. 3) The spatial difference of storms was relatively huge. The rainfall was much more in the east and the south than that in the west and the north. The rainfall in the northeast and the southeast accounted for 38.96% of the total. 4) The storms moving downstream and clockwise accounted for the most amount of rainfall of 57.94% and 81.61% runoff discharge and 84.84% sediment yield. Most of storms started from the northwest of the basin and moved downstream. When the process of rainfall was similar, the storm moving upstream had a fast hydrological response and a low peak flow and sediment yield. On the contrary, the storm moving downstream had a slow hydrological response and a high runoff and sediment yield.[Conclusions] The spatial and temporal distribution characteristics of storms have impact on the hydrological response of watershed, which is significantly reflected in the hydrological process and sediment yield. This result may provide a basis for understanding the complex interactions between rainfall variability and catchment heterogeneity.
2023 Vol. 21 (4): 69-78 [Abstract] ( 80 ) [HTML 1KB] [PDF 2833KB] ( 185 )
79 XIE Yangyang, LIU Xuyang, JIN Qiang, HUANG Jiafang, HEI Jie, LIN Shaoying, HUANG Zhuang, HOU Ning, WANG Weiqi
Characteristics of soil carbon, nitrogen, phosphorus and their ecological stoichiometric ratios in different habitats of East Lake Wetland, Fuzhou
[Background] Human activities and reclamation lead to the degradation of Fuzhou East Lake Wetland. The stoichiometric ratios of soil C(carbon), N(nitrogen) and P(phosphorus) not only reflect the cycling process of C, N and P, but also is a predictor of C, N and P saturation limitation. Studying the characteristics of soil C, N, P and their stoichiometric ratios in different habitats is helpful to understanding the limitation of land nutrients and has guiding significance for the rational utilization, protection and restoration of wetland resources in this area.[Methods] This study selected the four wetland habitats of bare tidal flat, abandoned breeding pond, Phragmites australis wetland, and shelter forest, five replicates were collected from each habitat, and 0-15 cm of topsoil was collected to measure the contents of soil C, N, and P and their ecological stoichiometry characteristics, as well as the relationship between them and soil physicochemical factors was analyzed.[Results] 1) Contents of both soil C and N were basically in the order of shelter forest > P. australis wetland > abandoned breeding pond > bare tidal flat (P<0.05) whereas soil C and N contents in the shelter forest were 13.99 and 1.47 g/kg. Yet soil P content was basically in the order of shelter forest > abandoned breeding pond > bare tidal flat > P. australis wetland (P<0.05), while soil P content in the shelter forest was 0.33 g/kg. 2) The regression fitting degree between soil C and N in four wetland habitats was high (R=0.98, P<0.05). 3) Soil C/N were basically in the order of the P. australis wetland > shelter forest > abandoned breeding pond > bare tidal flat, while C/P and N/P in the soils were significantly (P<0.05) in the order of P. australis wetland > shelter forest > bare tidal flat > abandoned breeding pond. 4) Soil environmental factors had a certain effect on C, N, P, and their stoichiometric ratios, as there were various correlations between soil C and density (R=-0.45, P<0.05), soil P and density (R=0.64, P<0.01), soil P and pH (R=0.67, P<0.01), soil P and water content (R=-0.73, P<0.01), soil C/N and density (R=-0.45, P<0.05), and electrical conductivity (R=-0.52, P<0.05); soil N/P and water content (R=0.82, P<0.01), soil N/P and with density (R=-0.88, P<0.01), and soil N/P and pH (R=-0.66, P<0.01).[Conclusions] Shelter forests regulated the changes of soil C, N, P and their ecological stoichiometric ratios in various wetland habitats, and contributed the most among the four wetland habitats. Our findings are of great significance in shelter forest for clarifying regulating variations of soil C, N, and P, as well as and their ecological stoichiometric ratios in various wetland habitats. This provides a scientific basis for the protection and restoration of key wetland ecosystems.
2023 Vol. 21 (4): 79-90 [Abstract] ( 84 ) [HTML 1KB] [PDF 4210KB] ( 148 )
 
Applied Studies
91 QIN Jianmiao, YANG Zhi, CHENG Jinhua
Multiple-time scales characteristic and change of water and sediment in Weining irrigated watershed
[Background] The Weining irrigated watershed, located at the main confluence of the Yellow River and Qingshuihe river in Ningxia, boasts abundant water resources and unique irrigation conditions. Despite its importance, few studies have been conducted on water and sediment in this region of China. By elucidating the trends, sudden change years, and cycle patterns of water and sediment in the Weining irrigated watershed, we can provide more robust support for regional decisions on soil and water conservation and subsequent irrigation in the basin.[Methods] We collected hydrological station data, including average daily runoff and average daily sediment volume, at the confluence of two major river sections in the Weining irrigated watershed. After normalization and other preprocessing, we analyzed water-sediment changes in the Weining irrigated watershed from 1989 to 2019 using distance level analysis, Mann-Kendall (M-K) test, and wavelet variance analysis. Preliminary conclusions regarding the water-sand trend and overall trend direction can be drawn through distance level analysis. M-K test, when combined with the overall trend direction obtained from distance level analysis, can identify potential mutation points (years) of water-sediment. Furthermore, wavelet variance analysis can elucidate the cyclical nature of water-sediment change.[Results] 1) The water-sediment variation pattern in the Weining irrigated watershed showed an oscillating trend prior to 2012. However, after 2012, the water and sediment trends diverged. The runoff volume gradually increased and remained above the average value of total runoff, while the sediment volume gradually decreased and remained below the average value of total sediment. Consequently, the overall trends of water and sediment were opposite, with a weak increase in runoff and a significant decrease in sediment. 2) During the 31-year period from 1989 to 2019, different numbers of mutation points for runoff and sediment volume were observed in the Weining irrigated watershed, corresponding to different numbers of mutation years. The M-K test showed that there should be several mutation points of annual runoff in the study area, but all of them did not reach the significance level, thus the actual mutation point was 0 and the mutation year did not exist, while there was one mutation point of annual sediment volume and it reached the significance level, combined with the trend direction of the distance level analysis, it was identified as the actual mutation point and the corresponding mutation year was 2005. 3) The water and sediment cycle pattern during this period also differed. The annual runoff cycle had a nested structure of "large-medium-small", with "large" corresponding to a 15-year cycle, "medium" to a 9-year cycle, and "small" to a 6-year cycle. It can be inferred that the annual runoff followed a similar general pattern in 15-year units, with the second and third main cycles of 9 and 6 years respectively controlling annual runoff under 15 years. The annual sediment volume demonstrated a single cycle pattern of 6 years, with sediment volume varying in 6-year units between 31 years. The number and magnitude of cycles for annual runoff and sediment volume suggested that the water and sediment variation patterns were similar on a short time scale of 6 years. However, when extended to 9 or even 15 years, the trends direction of water and sediment diverged.[Conclusions] There are many factors affecting runoff and sediment of basin, such as land use change, key water-control project and so on. Large human activities like water conservancy facilities will greatly alter underlying surface conditions and thus lead to a greater impact on water and sediment than climate change. In this study, results also show that water and sediment in study basin will decrease first and then increase in the next 6 years due to operation of The Shapotou Control Project.
2023 Vol. 21 (4): 91-99 [Abstract] ( 67 ) [HTML 1KB] [PDF 2707KB] ( 123 )
100 LIN Na, PAN Peng, WANG Bin, ZHANG Di, FENG Shanshan, PAN Jianping
Soil erosion rate calculation based on Stacking ensemble learning and leading factor analysis: A case study of Fengjie county in the Three Gorges Reservoir Area
[Background] The calculation and assessment of soil erosion is the key to soil and water conservation. In order to improve the calculation accuracy, stacking ensemble method is introduced, which can fully integrate different machine learning models to obtain high-precision spatial distribution data of soil erosion rate. At the same time, the leading factors affecting the soil erosion rate in the study area were analyzed.[Methods] Firstly, the feature dataset was constructed based on the data of 2018 rainfall, remote sensing images and others in Fengjie county, Chongqing, and the actual data of soil erosion rate in Fengjie county was used as the benchmark to train different machine learning models. Then, the accuracy evaluation index and diversity measure were used to establish the optimal combination of base-learners and meta-learner, construct the stacking integrated model, and to calculate the soil erosion rate in the whole county. Finally, the marginal dependence of the leading factors was analyzed according to the distribution law of soil erosion rate.[Results] 1) The stacking ensemble model with light gradient boosting machineand random forest as the base-learners and linearregressionas the meta-learner has the best effect. The MAE(mean absolute error), RMSE (root mean square error) and accuracy of R2(R-squared) are as follows:252.48 t/(km2·a), 537.78 t/(km2·a) and 0.868 7. 2) Elevation, rainfall, vegetation cover, slope, distance from the road and distance from water source were the top 6 factors influencing soil erosion rate in Fengjie county,with importance accounting for more than 9%. 3) Soil erosion rate was higher in the region with an elevation of 200-520 m, annual rainfall higher than 1 250 mm, NDVI (normalized difference vegetation index) of 0.24-0.27, slope of 26°-35°, distance from the road to 0-220 m, and distance from the water source to 63-387 m.[Conclusions] The results show that the stacking model constructed in this paper can effectively integrate different models and improve the accuracy of predicting soil erosion rate. Soil erosion rate in Fengjie county is affected by many factors.In general, soil erosion rate was positively correlated with elevation and vegetation cover degree, and negatively correlated with rainfall and slope.The higher rate of soil erosion tended to occur in steep low-elevation areas with abundant rainfall, low vegetation cover, and close proximity to roads and water sources.
2023 Vol. 21 (4): 100-112 [Abstract] ( 85 ) [HTML 1KB] [PDF 6681KB] ( 173 )
113 LI Xin, SHI Mingming, CAO Longxi, CHEN Guo, WANG Yun, YAO Lianfu
A composite fingerprinting analysis of sediment sources in a construction-disturbed small watersheds of Southeast Tibet
[Background] Construction activities such as transport projects may promote social development.However, it could also lead to serious soil erosion and environmental problems. In recent years, intensive engineering and construction activities have been conducted in the middle Yarlung Zangbo River basin in southeastern Tibet, China. Consequently, the local fragile ecological environment has been seriously disturbed. Quantitative analysis and theoretical support for erosion control and engineering disturbance evaluation is urgently needed. A composite fingerprint study about the contribution of soil loss from construction disturbance and its spatial variation can be helpful in engineering planning and assist the optimal deployment of conservation measures.[Methods] Soil samples were taken from potential erosion sources including woodland, grassland, slag, road cutting and unpaved roads. Sediment samples were taken from riverbeds, and totally 18 physical and chemical parameters were measured. The best fingerprint combination of K2O, Na2O, CaO and Cr was selected using Kruskal-Wallis H test and multivariate stepwise discriminant analysis. A multivariate linear mixed model was used to analyze sediment contribution rate of each erosion source. The quantitative relationship between sediment transport distance and contribution rate was established to reveal its spatial variation.[Results] The best fingerprint factors combination reached an overall correctly classified percentage of 94%for the total source soil samples. The average sediment contribution of the three main soil loss sources was ranked as:Road and side slope (61.61%) > slag site (21.15%) > natural woodland and grassland (17.24%). The average value of goodness of fit (GOF) was calculated as 0.867. The results showed that soil erosion from engineering disturbance was the main source of sediment that deposited in riverbeds of the small watershed. The sediment contribution rates of the two engineering disturbance sources showed different spatial variability. Sediment from the spoil site followed a linear decline trend of contribution rate along the river, with a critical impact distance of approximately 2 800 m. On the other hand, road cutting which generally parallel to the river continuously contributed to deposited sediment along the river. The road-related sediment contribution rates were high within a range of 220 m from the road. Outside this range, the contribution rate would decay exponentially as the distance between the road and the river increases. The effective road influence distance on deposited river sediment could be estimated as approximately 400 m.[Conclusions] The results of this study show the profound impact of engineering disturbance on erosion and sediment production in a small watershed of Southeast Tibet. It revealed the difference in sediment contribution variation of linear road and slag site. Empirical equations were established to predict the potential impact range of engineering disturbance on local watershed sedimentation.
2023 Vol. 21 (4): 113-122 [Abstract] ( 98 ) [HTML 1KB] [PDF 5457KB] ( 180 )
 
Development Studies
123 JIN Xinhong
Method of assisting soil and water conservation monitoring by using Ovitalmap
[Background] Surface disturbance caused by production and construction projects is the main source of soil and water loss caused by human activities. In China, 25,000 to 30,000 soil and water conservation projects are approved every year. The competent departments of the industry mainly obtain the relevant information of the projects through paper reports, and the supervision tasks are large and the monitoring data acquisition lags. The purpose of this study is to use new technical means to assist the monitoring of soil and water conservation, improve the efficiency of supervision and management of soil and water loss in projects and the accuracy of monitoring data, and reduce the soil and water loss caused by man-made construction activities.[Methods] In this study, Ovital map, CAD, ArcGIS software and mobile terminals loaded with Ovitalmap were used to carry out soil and water conservation monitoring for production and construction projects. The technical path was divided into four aspects, which are the project area soil erosion background investigation, soil and water conservation monitoring during the construction period, daily monitoring data management, water and soil erosion hazards emergency response.[Results] Compared with no Ovital map, this method:1) improved the accuracy of soil and water loss background survey data in the project area, and the data could be shared with other members in real time to carry out related work simultaneously; 2) it can quickly anticipate the area prone to soil and water loss in the construction process, so as to facilitate monitoring and improve work efficiency and monitoring results accuracy; 3) Ovitalmap, as data reported to management platform, facilitates the competent departments to carry out daily supervision and management; 4) Using maps to verify remote sensing results can improve the disposal efficiency of soil erosion hazards.[Conclusions] The use of Ovitalmap to assist soil and water conservation monitoring is beneficial to quickly and accurately obtain soil and water conservation monitoring data of production and construction projects, to improve work efficiency and data accuracy, and gradually realize the "one map" management of various topics with the help of this method, to provide diversified supervision and verification methods for the supervision of industry authorities, and provide an open participation platform for the masses to participate in and supervise the soil erosion of projects. Finally, it can improve the efficiency of supervision and management of soil and water loss in production and construction projects and reduce soil and water loss. Some functions of Ovitalmap require users to pay fees, and the map has weak statistical summary and overlay analysis of geographical factor attribute data, so it is recommended to optimize.
2023 Vol. 21 (4): 123-131 [Abstract] ( 120 ) [HTML 1KB] [PDF 10940KB] ( 214 )
132 ZHANG Yubo, ZOU Guofu, YANG Jiqing, SUN Xining, LI Xinyi, WEI Qingxi, LEI Ping, LI Bolin
Experimental study on the preparation of ecological restoration base material and planting performance on alpine rocky slope
[Background] The excavation of mineral resources has formed a large number of rock slopes,the rock surface is exposed and severely weathered,with serious soil erosion and inducing a series of ecological and environmental disasters such as geological disasters in mines.Good ecological substrate can well suppress soil erosion and restore the ecological environment.[Methods] In order to prepare an ecological substrate with good plant growth performance, strong soil and water conservation ability and suitable for ecological restoration of rocky steep slopes in alpine regions, the ecological slope protection base materials with different proportions were used by field base experiment, trolley slope simulation test and multi factor orthogonal test. In order to better conform to the on-site construction process, the substrate layer was divided into structural layer and surface layer to carry out plant performance research respectively. Through comprehensive seed germination rate and plant growth, the plantation performance of the substrate was evaluated.[Results] The extremely poor analysis found that when the pottery grains and walnut shell particles in the substrate structure layer were 7.50 g each, the grain husks and straw nodes of 2.50 g and 1.25 g respectively, the EPS of 0.10 g, the soil conditioner PAM of 1.50 g, and the water retention agent took 0.50 g, the plantation performance of the substrate structural layer was the best. The primary and secondary relationship of the influenc on the growth of tall fescue in the structural layer substrate was:ceramsite, walnut shell>soil conditioner PAM>chaff, straw>EPS>water retaining agent. When the straw was 2.50 g, the chaff was 7.50 g, the EPS was 0.30 g, the soil conditioner PAM was 0.40 g, and the water retaing agent was 0.20 g, the planting performance of the substrate surface was the best. The primary and secondary relationship of the influence on the growth of tall fescue in the surface layer substrate was:straw >water retaining agent>chaff>soil conditioner PAM>EPS.[Conclusions] Through the experimental study of the planting performance of ecological slope protection substrates, it provides an ecological slope protection substrate with simple preparation process,excellent plant growth performance andstrong soil and water conservation ability for the ecological restoration and water and soil conservation of rock steep slopes in alpine and altitude mines, and provides technical support for the ecological environment restoration of rock slopes in Northwest Yunnan.
2023 Vol. 21 (4): 132-143 [Abstract] ( 98 ) [HTML 1KB] [PDF 9800KB] ( 180 )
 
Forum
144 JIANG Dewen
Innovation and leading in soil and water conservation for Yangtze River Delta and Pearl River Delta in the New Era
[Background] The State Office of the State Council of the People's Republic of China has issued the"Opinions on Strengthening Soil and Water Conservation Work in the New Era". All provinces and industries are working out implementation plans. As China's leading regions in reform and development, the Yangtze River Delta and the Pearl River Delta should stand at a higher position, have forward planning, and play a leading role.[Methods] Here author presented his visions based on own long-term working experiences and accurate understanding on this topic.[Results] 1) The goal of regional soil and water conservation should be changed from quantity to quality with comprehensive improvement of water and soil conservation function and ecological product in following ways. Focusing on river network, we should maintain and promote the good function of ecosystem, and innovate urban soil and water conservation. We should promote high-quality development of economy and high-level protection of ecological environment with a focus on strict control of man-made water and soil erosion. We should promote rural revitalization and common prosperity by focusing on improving quality and efficiency. We should focus on improving the ecological value of soil and water conservation and carbon sequestration to serve the construction of an ecological civilization in the new era. We should speed up the modernization of governance systems and capabilities with the focus on improving management capabilities and standards. 2) We should innovate systems and mechanisms, promote smart soil and water conservation, and build a modern social service and management system. It can be done by the following ways. We should create a more open and efficient world-class business environment, and efficiently serve society. We should innovate the self-restraint and trustworthy mechanism of construction institutions, reducing the illegal behavior and soil erosion from the source with the high-grade soil and water conservation credit level. We should innovate the smart application of big data, the Internet, cloud computing, artificial intelligence, blockchain and the Internet of Things in the management of soil and water conservation, so as to enhance work efficiency in an all-round way. We should innovate the mechanism for social civilization and progress, increase the cognition level of soil and water conservation and ecological protection in an all-round way, and build and share with the whole society.[Conclusions] The innovation and leading in soil and water conservation in Yangtze River Delta and Pearl River Delta can be conducted in the new era.
2023 Vol. 21 (4): 144-149 [Abstract] ( 76 ) [HTML 1KB] [PDF 755KB] ( 198 )
 
Review
150 PENG Xudong, DAI Quanhou
Erosion environmental characteristics of surface erosion/underground leakage in the rocky desertification area, Southwest China
[Background] It has formed a unique surface and underground dual erosion environment system under long-term karstification in the karst area of Southwest China. The inlaid distribution of exposed bedrocks and soils in the rocky desertification area with the obvious bedrock exposed shapes the most complex system of erosion environment in the karst area, which presents its uniqueness in the composition and action characteristics of erosion environment. However, there is still a lack of systematic understanding in the erosion environment compared with other geographical areas, such as the Loess Plateau area, the Northeast Black Soil Area, etc.[Methods] Based on the previous research results in the soil erosion through field investigations, positioning tests and indoor analyses in the rocky desertification area of Guizhou province, China, this paper deeply analyzed and summarized the compositions of the dual erosion environment, the erosion objects, the erosion types, the erosion dynamic factors and action characteristics on surface erosion or underground leakage loss in the rocky desertification area.[Results] The erosion environment has typical characteristics of vulnerability, complexity and variability in the area. In terms of composition, the erosion environment can be divided into three aspects:erosion power, erosion object and erosion interface. The erosion power includes external forces such as water power (rainfall, rock surface flow and surface runoff), gravity and human factors, as well as internal forces such as karstification and rocky desertification. The erosion objects include soil, humus, rock and rock weathering. The erosion interface includes surface and underground, soil-rock interface, water-soil interface, water-rock interface, rock/soil gas interface and rock/soil biogenic interface, etc. In this unique erosion environment background, the soil erosion in this area presents a dual erosion mechanism of surface erosion and underground leakage. The surface erosion mostly occurs in the form of water erosion, while the underground leakage superimposes the coupling effect of water erosion, gravity erosion and chemical dissolution. Finally, the key points and suggestions for soil erosion research are discussed in the karst rocky desertification area.[Conclusions] Future research on the soil erosion in the karst rocky desertification areas needs to focus on the action mechanism of erosion dynamic system and erosion interface system on soil surface erosion and underground leakage, and further clarify the occurrence process, mechanism and influencing factors of various types and forms of soil erosion, especially the formation causes, distribution areas and sensitive influencing factors of gravity erosion such as karst collapse, which is easy to cause disasters, and then establish the theoretical system of surface erosion or underground leakage resistance control. This study is helpful to deepen the understanding of erosion environment, and provide theoretical reference for the study of surface erosion/underground leakage in the rocky desertification area.
2023 Vol. 21 (4): 150-158 [Abstract] ( 92 ) [HTML 1KB] [PDF 3848KB] ( 165 )
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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