中国水土保持科学
中国水土保持科学
 
 
 
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2021 Vol.19 No.3  Published 2021-06-30
  
 
Foundamental Studies
1 SHI Ruoying, ZHU Qingke, LI Yixuan, GOU Qingping
The relationship between slope micro topography and community quantity characteristics in loess area of North Shaanxi province
[Background] The objective of this study is to grasp the relationship of plant community quantitative characteristics and various types of micro topography in the loess area of northern Shaanxi province, and this research has certain significance for the vegetation restoration and reconstruction on difficult sites in semi-arid loess area of northern Shaanxi province.[Methods] Based on the survey data of a series of plant community quantitative characteristics such as species composition, herbaceous biomass, vegetation coverage and vegetation diversity on 5 micro-topographies of Hegou valley in Wuqi county of northern Shaanxi province, including gully, collapse, platform, shallow gully, scarp and the undisturbed slope, the correlations between micro-topographies and plant community quantitative characteristics were analyzed. The data were processed via statistical analysis and significance test of difference.[Results] 1)The slope micro-topography has a significant impact on vegetation growth. There is a significant correlation between the micro-topography and the plant community quantitative characteristics like richness, herbaceous biomass, vegetation coverage, vegetation diversity and other indexes. 2)The plant communities on the various types of micro-topography are dominated by herbaceous communities. Among them, the plant community quantitative characteristics on different slope micro-topography of the semi-shady slopes are mostly superior to those on semi-sunny slopes, and the natural succession stage of the plant community is more advanced than semi-sunny slopes, too. 3)The characteristic of the species composition, herbaceous biomass, vegetation coverage and vegetation diversity of plant communities in various types of slope micro-topography are better than those on the undisturbed slope. Among them, two types of shrubs appeared in the gully, and the vegetation growth in the gully was the best, followed by the vegetation growth in the collapse, platform and shallow gully is slightly worse, while the vegetation growth of the scarp was the worst.[Conclusions] There is a certain relationship between the vegetation characteristics and the micro-topographies in the loess area of northern Shaanxi province. Different micro-topographies in loess area of northern Shaanxi province has caused the spatial differences of habitat conditions, which resulted in the significant differences in vegetation characteristics. Therefore, when vegetation restoration is carrying out in the loess area of northern Shaanxi province, the differences of plant community characteristics should be considered based on the characteristics of different micro-topographies, aiming to promote the guide for the vegetation restoration on difficult position in the loess area of northern Shaanxi province.
2021 Vol. 19 (3): 1-7 [Abstract] ( 308 ) [HTML 1KB] [PDF 874KB] ( 369 )
8 WANG Huiqin, SUN Baoping, YU Xinxiao, XIN Zhongbao, JIA Guodong
Spatio-temporal variations of soil erosion and its drivers in the northern region of North China
[Background] The ecological environment of Bashang Plateau and northern mountainous region in North China is fragile and soil erosion is serious, which potentially threatens the ecological security and sustainable development of this region and surrounding areas. The purpose of this study is to improve the understanding of soil erosion dynamic in the study area, and to provide scientific basis for comprehensive land management and improvement of soil and water conservation measures in the region.[Methods] We selected meteorological data, NDVI data sets and geo-related data from 1998 to 2015, and applied the USLE, RWEQ model and trend analysis to study the soil erosion dynamics in the region and its influencing factors of spatiotemporal distribution and change trends.[Results] 1) The distribution of soil erosion in the study area changed from wind erosion to water erosion from northwest to southeast. During 1998-2015, water erosion decreased significantly. Although wind erosion increased somewhat since 2008, the overall trend decreased and only a small part of the study area was intensified. 2) Soil and topography reflected the spatial differences for soil erosion. The northwest part in the study area is flat with high elevation, while southeast part is undulating with multi-gradient slope factor and its main soil types with relatively high soil erodibility. 3) Rainfall erosivity and wind force were the important driving factors for soil erosion, with strong spatiotemporal differences. Rainfall erosivity generally increased from 1998 to 2015, while overall trend of weather factor showed a slight downward trend. During the period from 1998 to 2015, fraction vegetation cover increased significantly.[Conclusions] With the increase of fraction vegetation cover, the overall soil erosion gradually decreases, and the vegetation restoration project in the sandstorm source area of Beijing and Tianjin plays an important role.
2021 Vol. 19 (3): 8-18 [Abstract] ( 450 ) [HTML 1KB] [PDF 9670KB] ( 668 )
19 WU Xueqin, XIE Yunhu, LIU Xiaoxi, DING Jing, HAI Chunxing
Grain size characteristics of sediment under four typical sand shrubs in the southeast edge of Tengger Desert
[Background] The oasis-desert transition zone is an ecologically sensitive and fragile zone in which deserts and oasis transform each other. How to choose sandy shrubs suitable for growing in this area is one of the hot topics for practitioner engaged in desert and oasis.[Methods] In the desert-oasis ecotone in the southeastern edge of Tengger Desert, the surface soil sediment samples of 0-5 cm at the roots, 50 and 100 cm from the roots of Artemisia desertorum, Nitraria tangutorum, Haloxylon ammodendron and Hedysarum scoparium, along the northwest, southwest, northeast and southeast directions were collected. Statistical methods were used to analyze the grain size composition and parameter changes of sediments under the shrubs, and spatial interpolation method to analyze spatial changes.[Results] 1) The composition of the surface soil sediments under the four shrubs was mainly medium sand; the grain-level content of the understory sediments was the same as that of A. desertorum and N. tangutorum, and the same for H. ammodendron and H. scoparium. 2) The average particle size of the sediment ranged from 1.39Φ-1.88Φ. The average particle size of the sediments under the N. tangutorum had no obvious change from the root to the periphery, and the particles were finer compared with the other three shrubs. The selectivity was medium, and the sediments of the other three shrub species were better. The skewness was negative and the kurtosis was medium peak. 3) Fine particles accumulated in the southwest direction under the A. desertorum forest, the northwest direction under the N. tangutorum forest, the southeast direction under the H. ammodendron forest, and the northeast direction under the H. scoparium forest. 4) Sediment grain size was significantly negatively correlated with plant height at 100 cm southwest of the four shrubs (P<0.05), and positively correlated with coverage at 100 cm northwest (P<0.05).[Conclusions] N. tangutorum as the main sandy shrub in the transition zone, its sand-fixing and soil-holding ability is higher than that of other sandy shrubs. The growth of shrubs is concentrated and clustered, and the protection range is larger than other sandy shrubs.
2021 Vol. 19 (3): 19-27 [Abstract] ( 415 ) [HTML 1KB] [PDF 9895KB] ( 567 )
28 XU Wenxu, YANG Xiankun, CUI Bin, XU Ziqi
Analysis of the soil thickness and the degradation degree of the typical slope farmland in the black soil region of Northeast China
[Background] The degradation of the sloping farmland in the black soil region not only reduces the quality of the land and the water resources, but also causes the deterioration of the ecological environment. This study explores the change rule of the soil thickness and the degradation of the sloping farmland in the black soil region of the Northeast China, and it provides theoretical foundation for the prevention and control of the soil erosion on sloping field.[Methods] 6° and 10° sloping farmlands in Dongliao county of Jilin province were selected as the main research objects, and a 8° farmland with soil and water conservation measures implemented in the near area was as CK field. We studied the degree of soil erosion by measuring the thickness of soil and investigated the degradation at different slope positions on the slope farmland in the black soil region via corresponding mechanical and chemical methods. We employed Excel,SPSS20.0, ANOVA to process data and cluster analysis for the classification of the soil degradation.[Results] 1) The place with cultivated soil layer of 20 cm was the critical point, and when the soil thickness was <20 cm, it meant that the soil erosion was strong on this sloping position. 2) The soil physical and chemical properties and the soil thickness statuses of the 6°slope and the 10° slope were significantly worse than those of the CK field(P<0.05), and the soil physical and chemical properties rank of the 10° slope was as "bottom > top > middle", and the rank of the 6° slope was as "bottom > middle > top". 3) The thinner the soil thickness was, the worse the physical and chemical properties and the yield were, that meant the more serious the erosion was, the more serious the degradation was. 4) The soil degradation degree of the 6° slope and 10° in the study area were classified into 5 types, type 1 was characterized by the slight erosion and the relative high yield; type 2 was characterized by the low moisture content and the low rapidly available phosphorus and rapidly available potassium content; type 3 was characterized by the high bulk density, the low organic matter content; type 4 was characterized by the good soil physical and chemical properties and the high yield, and type 5 was characterized by the low moisture content, the high bulk density, the low nutrient content and the low yield.[Conclusions] The reduction degree of soil thickness and the degradation degree in the study area are relatively serious,and the reduction and degradation rule between the 10° slope and the 6° slope are different, and the results may provide theoretical support for the prevention and control of the degradation of the sloping farmland in the black soil region.
2021 Vol. 19 (3): 28-36 [Abstract] ( 649 ) [HTML 1KB] [PDF 2010KB] ( 345 )
37 HUANG Kai, LI Rui, YANG Pingping, PAN Lidong, ZHANG Linqing
Distribution characteristics of soil total organic carbon in typical Karst area and its response to different planting and management modes of slope farmland
[Background] Karst landforms are concentrated in the southwest of China. Under the influence of both natural and human factors, rocky desertification is serious in this area. The total organic carbon (TOC) content is an important index to reflect the soil quality. Compared with traditional planting mode, compound planting mode may reduce soil erosion and improve TOC. The purpose of this paper is to explore the distribution characteristics of TOC in typical Karst rocky desertification areas and the change patterns of TOC under different planting and management modes.[Methods] Qianxi Jinlan demonstration area and Guanling-Zhenfeng Huajiang demonstration area were taken as study areas. The two study areas are of strong typicality in rocky desertification degree and slope farmland planting modes. Based on the field sampling and laboratory analysis, the intrinsic mechanism of TOC changing with the degree of rocky desertification and the response mechanism to different planting and management modes were discussed.[Results] 1) The average TOC of Qianxi Jinlan demonstration area was 29.06 g/kg. The average TOC of Guanling-Zhenfeng Huajiang demonstration area was 33.02 g/kg. There was no significant difference in TOC content between the two study areas. 2) The TOC of intensive rocky desertification was the highest, which was 38.96 g/kg. There was a significant difference in TOC content between moderate rocky desertification and intensive rocky desertification (P<0.05). 3) The TOC content in different planting modes showed the following pattern:silvopasture (34.38 g/kg) > agroforestry (33.35 g/kg) > economic fruit forest (32.23 g/kg) > cultivated pastures (30.91 g/kg) > monoculture of other crops (27.20 g/kg) > maize (17.67 g/kg). 4) There was a significant difference in TOC content among 3 field management modes (refined management, general management, and extensive management) in slope farmland. With the increase in the delicacy of field management mode, TOC content showed a trend of increasing gradually.[Conclusions] Compared with non-karst areas, the TOC content of topsoil in Karst area is not low. With the aggravation of rocky desertification, the TOC of soil will not always decrease. Planting and management modes have a great impact on TOC. In general, compound planting, grass planting, afforestation, and refined management may significantly improve the content of TOC in slope farmland. The results of this paper may provide a theoretical basis for the adjustment of the planting structure in the Karst slope farmland, and the comprehensive control of regional soil erosion and rocky desertification.
2021 Vol. 19 (3): 37-46 [Abstract] ( 420 ) [HTML 1KB] [PDF 1479KB] ( 327 )
 
Applied Studies
47 WEI Yangchen, LI Shiyu, YANG Jianying, ZHAO Tingning, WANG Ying, WANG Anyi
Effects of salt stress on the growth and physiological characters of 6 typical greening tree seedlings in Tianjin coastal saline-alkali land
[Background] Tianjin Binhai New district is the first national comprehensive reform and innovation zone in China, but its land is severely salinized. This problem restricts its saline-alkali land reclamation and ecological restoration, resulting in serious soil erosion problems, which is not conducive to its sustainable economic,social and ecological development. Therefore, based on the soil and plant conditions in the coastal saline-alkali area of Tianjin, this study selected 6 representative greening trees in North China to explore their physiological salt tolerance mechanisms and to conduct a comprehensive salt tolerance evaluation. This study aims to add alternative greening trees to the saline-alkali area of Tianjin Binhai New district, and to improve the level of green landscape in the process of ecological restoration in this area.[Methods] Six greening tree seedlings (Albizia julibrissin, Hibiscus syriacus,Amorpha fruticosa, Lycium barbarum,Lonicera maackii, and Parthenocissus tricuspidata) commonly used in North China were selected as test materials, and a gradient design of 4 NaCl solution concentrations of 0.2%-0.5% was simulated to calculate the growth and physiological indexes of different tree seedlings under salt stress, and the membership function method was adpated for the comprehensive evaluation of the salt tolerance of 6 tree seedlings.[Results] 1) A. fruticosa, H. syriacus and A. julibrissin were all alive after 15 d of salt stress at each concentration. L. barbarum, L. maackii and P. tricuspidata were alive with the increase of concentration and the number of cultivation days, their survival rates decreased, and P. tricuspidata cultivated at 0.5% concentration all died after 15 d. 2) With the increase of salt concentration, the biomass of A. fruticosa increased firstly and then decreased, and the biomass of other trees decreased. Under the 0.2% and 0.3% concentration, the aboveground biomass of A. fruticosa increased, and the belowground biomass of H. syriacus increased. 3) Under salt stress, the relative conductivity, MDA and soluble sugar content of the 6 tree seedling leaves increased. The soluble sugar content of L. maackii changed the most. The soluble sugar content of P. tricuspidata vulgaris reached the peak at 0.3% and then decreased.[Conclusions] The growth of L. barbarum is the most sensitive to salt stress, and the growth of A. fruticosa is promoted under 0.2% and 0.3% salt stress. The aboveground part of H. syriacus is more sensitive to salt stress, and the underground part of A. fruticosa is more sensitive to salt stress. A. fruticosa and A. julibrissin showed a more stable cell membrane structure and function under salt stress. P. tricuspidata had a disordered osmotic regulation function of soluble sugar from 0.3% salt stress, and the cell membrane structure was severely damaged.The comprehensive salt tolerance of 6 greening tree seedlings was A. fruticosan > H. syriacus > A. julibrissi > L. barbarum > L. maacki > P. tricuspidata.
2021 Vol. 19 (3): 47-55 [Abstract] ( 341 ) [HTML 1KB] [PDF 988KB] ( 355 )
56 ZHAO Danyang, BI Huaxing, HOU Guirong, CUI Yanhong, WANG Ning, WANG Shanshan, MA Xiaozhi
Evolution of vegetation and soil nutrients of artificial Robinia pseudoacacia forest
[Background] Robinia pseudoacacia is one of the tree species with the largest afforestation area in the loess region of western Shanxi province. However, as the forest age increases, due to factors such as soil moisture and nutrients, the R. pseudoacacia forest has experienced varying degrees of degradation. To explore the change characteristics of undergrowth vegetation and soil nutrients in the restoration process of artificial R. pseudoacacia forest, the 18, 22, 26, 31 and 36 years artificial R. pseudoacacia forests in the loess region of western Shanxi province were taken as the research objects in this study.[Methods] The method of spatial sequence instead of time successional sequence was adopted, and one R. pseudoacacia plot of 20 m×20 m, 5 shrub plots of 5 m×5 m, and 5 shrub plots of 1 m×1 m were selected in forests of different ages with similar site conditions. Then vegetation growth indicators were investigated, soil profiles were excavated, and soil samples were collected to determine soil nutrients indicators, then correlation analysis were conducted, so as the change characteristics of growth of R. pseudoacacia forest, undergrowth vegetation and soil nutrients with stand age were clarified.[Results] 1) With the increase of the age of R. pseudoacacia forest, the average DBH and height of the trees increased gradually, and the average crown diameter increased first and then decreased. 2) The soil nutrient content of R. pseudoacacia forest land with different ages tended to gather on soil surface, the soil nutrient content of the forest land decreased with the increase of the depth of the soil layer, and content in the soil layer with 0-10 cm was significantly higher than that in the soil layer below 30 cm (P<0.05), in which the vertical spatial distribution of organic matter content and total nitrogen content was similar to changes with forest age; the content of soil organic matter, total nitrogen and total phosphorus in the forest lands increased first and then decreased with the increase of R. pseudoacacia stand age, but the increase trend of soil available nitrogen was not obvious, and the content of soil available phosphorus decreased. 3) With the increase of R. pseudoacacia stand age, the number of undergrowth vegetation species increased, and the height and coverage first decreased and then increased. In addition, the growth of undergrowth vegetation was affected by the growth characteristics of R. pseudoacacia and soil nutrients. The restoration of R. pseudoacacia forests had an impact on the undergrowth vegetation and soil nutrient. R. pseudoacacia forests improved soil nutrients, but at a certain stand age, this effect was weakening.[Conclusions] The growth of R. pseudoacacia forest has a certain effect on improving soil nutrients. The 26 years old forest performed better overall. This study reveals the changing laws of vegetation and soil nutrients in the R. pseudoacacia forest during the growth process, and the results are conductive to understanding the overall characteristics of the artificial R. pseudoacacia forest in the area, and it may provide a scientific basis for vegetation restoration and the management of the R. pseudoacacia forest, and then improve the stability of the ecosystem in this area.
2021 Vol. 19 (3): 56-63 [Abstract] ( 490 ) [HTML 1KB] [PDF 1021KB] ( 321 )
64 DAI Qiao, LIN Jie, ZHU Yanfang, PAN Ying, DONG Bo, XU Yanyin
Remote sensing inversion of vegetation cover management factor based on the southern structured vegetation cover index
[Background] The C-factor estimation models cannot be used universally used in northern and southern China due to the influence of spatial heterogeneity. A review of current literature suggests that there is a lack of research on the vertical structure of forest water and soil conservation in southern China. Therefore, the objective of this research was to explore the best estimation model of C factor at different scales based on the Southern Structured Vegetation Index (Vs). Nanjing is a typical subtropical hilly area with abundant vegetation.[Methods] This study investigated a total of 87 typical quadrats (six land use types) from 16 mountains in 8 districts of Nanjing. The quadrats were arranged according to the principle of uniform spatial distribution. The data including the longitude and latitude, elevation, slope, slope position, land use, litter layer thickness, tree species, shrub, grassland and tree height of the sample plot recorded in detail. The remote sensing index was extracted from the corresponding remote sensing images. The Vs of different vegetation types was fitted with the C value to obtain the C factor prediction model. At the regional scale, the best remote sensing index was selected by Vs, then the C factor was retrieved by remote sensing.[Results] 1) C-factor estimation based on Vs effectively improved the accuracy of the model. 2) Factor C showed an increased sensitivity to yellowness index and as a result the protective effect of senile vegetation and dead leaf cover on surface soil cannot be ignored. 3) Inversion of C factor based on the optimal remote sensing index, model R2=0.598, ME>0.5, and thus this model is recommended for estimation of C factor in large scale.[Conclusions] In the southern region, the C-factor of slope scale estimated by Vs is more accurate. At the regional scale, the remote sensing index based on Vs screening can effectively invert the vertical information of vegetation to the remote sensing index. This is the first reported study focusing on the structured vegetation index in southern China.
2021 Vol. 19 (3): 64-71 [Abstract] ( 472 ) [HTML 1KB] [PDF 2167KB] ( 485 )
72 QIU Dexun, ZHAO Baili, YIN Diansheng, MU Xingmin, GAO Peng
Vertical variation of soil moisture in the loess hilly and gully region and its influence factors
[Background] Soil moisture (SM) is one of the key factors for plant growth and eco-environment reconstruction on the Loess Plateau of China. Vertical variation of SM as affected by landform and land use was studied in the Zhifanggou watershed of Ansai county in Shaanxi province.[Methods] We selected 78 representative plots with four land use types in the whole watershed. Three sampling points were selected on the diagonal of each plot. The sampling depth ranged from 0 to 1 000 cm. A total of 40 samples were collected at each point by using a soil auger (10 cm intervals from 0 to 100 cm, 20 cm intervals from 100 cm to 500 cm, and 50 cm intervals from 500 cm to 1 000 cm). The average soil moisture, standard deviation and coefficient of variation of each layer were calculated. The effects of different factors on soil moisture were analyzed quantitatively by variance contribution rates. LSD multiple comparison and t-test were used to compare the differences of soil moisture under different conditions.[Results] 1) The vertical distribution characteristics of SM in 0-1 000 cm were different under different land use. With the increase of soil depth, the SM of the forest land decreased rapidly (0-50 cm) to 6%-9%. The SM of the bush land decreased first (0-50 cm) and then increased slowly. The SM of the abandoned grassland and the farmland increased gradually with the increase of soil depth, and finally stabilized. 2) In general, the longer vegetation age, the lower mean soil moisture. However, in the abandoned grassland, the trend was not obvious. 3) The SM in the shallow layer (0-200 cm):abandoned grassland (10.20%) > farmland (10.04%) > bush land (9.39%) > forest land (8.91%); in the deep layer (200-1 000 cm):farmland (13.50%) > abandoned grassland (13.34%) > bush land (11.66%) > forest land (7.87%). This indicated that the abandoned grassland maintained SM well, while the forest land was relatively poor. 4) The slope had a significant effect on the SM in the shallow layer of the abandoned grassland and the deep layer of the forest land. The steeper a slope was, the lower SM was observed. The aspect had a significant effect on the SM in the shallow layer of the forest land and the abandoned grassland, and the SM on the sunny slope was higher than the shade. On the whole, the SM and the coefficient of variation both decreased first and then increased, which showed a significant positive correlation. Land use, slope and their interaction had significant influence on the SM in shallow layer, the contribution rate of slope was the largest (34.85%), and land use had significant influence on the SM in deep layer, the contribution rate was 23.03%.[Conclusions] The SM in loess hilly and gully area had obvious vertical variation, and was affected jointly by land use, slope and aspect. Abandoned grassland may keep SM better, but forest land was relatively poor. Topography was an important factor affecting the variation of SM in shallow layer, while SM in deep layer was mainly affected by land use.
2021 Vol. 19 (3): 72-80 [Abstract] ( 465 ) [HTML 1KB] [PDF 3333KB] ( 317 )
81 LIU Yufei, ZHAO Yike, YANG Yuanjun, ZHANG Liyun, LIU Wujiang, XIONG Shoude, DUAN Qingsong
Effect of roots of two mixed sowing herbaceous plants on soil shear strength
[Background] Plant roots have a positive effect on improving slope stability and reducing soil erosion. Herbaceous sowing methods include single sowing and mixed sowing. Previous studies demonstrate that, compared with single sowing, mixed sowing is more beneficial to increasing the total coverage and the height of the grass belt,which in turn enhances the soil and water conservation effect. Therefore, the aim of this study is to explore effects and mechanism of mixed sowing herb roots in natural state improving shear strength of soil, so as to select a reasonable sowing method to strengthen the soil-fixing effect of herbaceous plants, and provide a scientific basis for ecological environment construction.[Methods] The experiment was carried out at the experimental farm of the Yunnan Agricultural University, China. In July 2017, a total of 40 PVC tubes, 51 cm in length, 110 mm in diameter and 3.2 mm in thickness, were all cut in half, and then the halves were bound together by pair with rubber bands. Upland red soil <5 mm in particle size was packed into the rubber-band-fixed tubes with the bottom sealed with plastic film up to 50 cm. The experiment was conducted with 4 treatments(10 samples for each):pure soil, Medicago sativa, Setariaanceps stapf ex massey, and mixture of M. sativa and S. stapf ex massey (1:1). Six seeds were put in each tube, separately. In October 2018, out of each group, 9 tubes were picked randomly, placed in water for 24 h until being fully saturated. Soil columns were taken out from the tubes. Shoots of the plants were cut off. The soil columns were cut into two, 25 cm for each. From each half of the soil columns, a section of 20 cm in the middle was taken as test samples and the section was 10.36 cm in diameter. The saturation density of the samples were tested. Unconfined shear strength was tested on a SJ-1A type strain controlling triaxial apparatus.[Results] :1) ΔC (cohesion increment) in the upper layer of root-soil composite of single M. sativa, single S. stapf ex massey and the mixed sowing were 10.85, 15.587 and 20.284 kPa, respectively; the cohesion of the respective root-soil composite was 125.93%, 180.90% and 235.42% of pure soil cohesion(8.616 kPa).ΔC of the lower layer were 5.134, 11.356 and 14.950 kPa, respectively; the cohesion of the respective root-soil composite was 62.82%, 139.04% and 183.04% of pure soil cohesion(8.168 kPa). 2) The results showed that 85.80% of M. sativa roots were >1 mm in diameter, thinner roots were larger than 0.2 mm; roots of S. stapf ex massey were <0.6 mm in diameter; roots of mixed sowing were in all observed diameter classes. 3) The relationship of ΔC with Rd (root density), Rar (root area ratio) and Q (root content in a column) was significant or extremely significant, and the correlation between ΔC and Q was the strongest.[Conclusions] The soil shear strength increment in the mixed sowing is higher than that in single sowing, which indicates that mixed sowing has better effect on soil and water conservation. The soil shear strength increment of the mixed sowing has fine correlation with Rd, Rar and Q, and the correlation with Q is the best. Thus, Q can be used to predict the soil shear strength increment of mixed herbaceous roots.
2021 Vol. 19 (3): 81-88 [Abstract] ( 419 ) [HTML 1KB] [PDF 943KB] ( 483 )
89 LIANG Zhishui, WU Zhiren, ZHANG Lixin, GAO Haiying
Resisting water impact performance of solidified sandy soil by W-OH
[Background] China is one of the countries facing the most serious soil erosion. Soil erosion is mainly caused by water erosion, which is mainly reflected in rain drop hitting and runoff erosion. The main control measures for this problem include forest and grass measures, engineering measures and farming measures. Recently, the measures of soil consolidation by materials have become a research trend because of their simple construction and remarkable soil consolidation effect, W-OH is a kind of hydrophilic polyurethane modified composite material, which is using water as curing agent. It can be applied for desertification control and water and soil conservation since it has excellent resistance to wind and rainfall erosion. The anti-scourability of the solidified consolidation layer has been studied in rainfall conditions but the flow impact performance is rarely reported now.[Methods] In order to study the effect of W-OH on the resisting flow impact performance of consolidated sandy soil, a simulated flow impact test was conducted under the conditions of W-OH concentration (3%, 4%, 5%, 6% and 7%), slope angle (0, 15°, 30°, 45° and 60°) and flow velocity (4, 5, 6, 7, 8, 9 and 10 m/s).[Results] The solidified sandy soil based on W-OH had good resistance to water and splash erosion. The ability of splash resistance became stronger with the increase of the slope angle. The range of the flow impact resistance time did not change much when the slope angle was <45°. The range of the flow impact resistance greatly increased when the slope angle was >45°. Thus, the resisting performance at the slope angle of 60° was about 11.3 times of that in the condition of vertical impact. Additionally, the splash resistance increased significantly when the concentration of W-OH increased. The destruction time in the condition of 7% W-OH was about 219 times than that in the condition of 3% W-OH and vertical impact when the slope was fixed in 60°. Fixing the flow impact time as 5 min, the destruction time of solidified layer decreased with the increase of flow velocity and there was a positively linear relationship with the critical flow velocity with different concentrations. Additionally, the impact of flow velocity on the solidified layer was significant, but the slope angle was less.[Conclusions] The results indicate that W-OH concentration has a significant effect on the impact resistance of solidified layer and W-OH can be used to solidify soil. This will provide a theoretical basis for the application of W-OH in the prevention and control of soil erosion.
2021 Vol. 19 (3): 89-94 [Abstract] ( 569 ) [HTML 1KB] [PDF 863KB] ( 401 )
 
Engineering Study
95 YANG Jianying, LIANG Dedong, SHI Changqing, WANG Huibo, LUO Guangtian, GONG Bo, YAN Jibin
Characteristics of runoff and sediment yield during artificial snow melting in ski slope
[Background] The density of artificial snow is much higher than that of natural one, the vegetation coverage of ski slope is low, and the feature of frozen-thawed soil has changed. After warming up in spring, the rapid melting of artificial snow will generate a large amount of melting water, and this will cause great soil erosion. Therefore, it is of great significance to study the runoff and sediment yield from artificial snow melting in ski slope. In order to study the characteristics of runoff and sediment yield from artificial snow melting on ski slope, this paper observed and studied the simple runoff plots in a field, which provides theoretical basis for ski slope construction and soil erosion control.[Methods] In this study, two runoff plots with the size of 2.5 m×10 m were set up on the intermediate ski slope of Beijing Shijinglong ski slope. Through the runoff plot observation method, the runoff flow and sediment concentration were measured and calculated in April 10 and 11, 2018, and sampled every hour.[Results] 1) Air temperature and soil temperature showed the change pattern of "Peak" type with time. The peak of temperature appeared at 14:00 and the peak of soil temperature appeared at 15:00. 2) There was a cubic function relationship between snow volume reduction and air temperature, but the fitting effect between snow volume reduction and soil temperature was not ideal. 3) The runoff flow and sediment concentration of snowmelt on the ski slope increased first and then decreased. Among them, the average runoff flow was 11.52×10-6 m3/s, the average sediment concentration was 0.30 kg/m3, and the average soil erosion modulus was 4 360 t/(km2·a), which belonged to moderate erosion. In addition, runoff flow and sediment concentration were also affected by soil, mulch and slope gradient, and the relationship between runoff flow and sediment concentration was linear.[Conclusions] Through experimental observation and analysis, it provides theoretical basis for ski slope construction and soil erosion control. More attention should be paid to surface soil improvement and vegetation construction of ski slope. The runoff and soil erosion caused from artificial snow melting can be reduced by improving the soil permeability and erodibility of ski slope. The construction of vegetation may increase the surface roughness and improve the physical and chemical properties of soil, thus it can play a role in preventing and controlling soil erosion.
2021 Vol. 19 (3): 95-102 [Abstract] ( 551 ) [HTML 1KB] [PDF 1090KB] ( 376 )
 
Development Studies
103 ZHANG Shuai, ZHAO Shulan, LEI Xiaozhang, FU Wenxi, CHEN Zhuo
Automatic identification of typical landslides in Baxie River Basin based on region growing
[Background] The Loess Plateau is prone to a large number of landslides under the condition of concentrated rainfall in summer, which causes huge damage to local people's lives and property, rapid extraction of landslide information plays an important role in disaster response. At present, there are a large number of landslides in the Baxie River Basin of the Loess Plateau, and most of them are typical landslide. Traditional manual interpretation can effectively identify landslides, but its efficiency is extremely low. In addition, due to the restrictions of terrain and weather, the manual interpretation of typical landslides is more difficult.[Methods] On study area Baxie River Basin in the Loess Plateau, using Google Earth software to extract the images of study area,and Gaussian filter was adopted to reduce the influence of image noise on recognition results. The gray value range of the trailing edge of the interpreted landslide in the study area was used as the condition for automatic selection of seed points, then using region growing algorithm and morphological operations to realize recognition and trailing edge boundary extraction of landslides in typical landslides that has not been interpreted in the study area. Optimal region growth conditions were obtained by adjusting the growth threshold.[Results] This method automatically identified the typical landslide in the study area.The combination of morphologic open operation and close operation removed the obvious sawtooth and small burrs in the results and link the external broken lines to smooth the edges. Sobel operator combined with watershed algorithm extracted effectively the landslide's trailing edge boundary. Correct identification, wrong identification and missing identification existed in the extraction process of landslide trailing edge boundary. With the increase of the growth threshold, the divergence factor increased and the error factor decreased, indicating that the over-recognition increased and the missing recognition decreased. Three images of the Baxie River Basin in the Loess Plateau were extracted by Google Earth. The three images were identified and the landslide trailing edge was extracted by this method. Meanwhile, the three images were interpreted manually and the landslide trailing edge was drawn to verify the identification results. When the gray growth threshold is 10, the accuracy of identifying the trailing edge of landslide reached 78.94%. For new landslides, the grayscale characteristics at the back edge of the landslide body were obvious, and the identification results were good. For landslides with a long occurrence time, the surface weathering and new vegetation growth will reduce the identification accuracy of this method.[Conculsions] These suggest that the proposed method is effective to identify the typical landslides in Baxie River Basin of Loess Plateau, which provides a direction for landslide disaster assessment, rescue and reconstruction.
2021 Vol. 19 (3): 103-109 [Abstract] ( 335 ) [HTML 1KB] [PDF 4672KB] ( 388 )
110 FANG Rui, XIN Huarong, GUO Xianjie, YOU Yinghua, LE Feng, WU Fang, ZHOU Zuyu
Function and practice of dynamic supervision system of soil and water conservation
[Background] The business requirements of dynamic supervision of soil and water conservation usually include three aspects:dynamic monitoring of regional soil and water loss, informatization supervision of production and construction projects and fine management of main projects. Due to the different requirements and purposes, the information and application results with different requirements are difficult to share, which brings difficulties to the unified supervision of water administrative departments at all levels. According to the business requirements of local government's dynamic supervision of soil and water conservation, and combining with the business logic and supervision experience of Ecological Environment Monitoring Station of Jiangsu Provincial Soil and water Conservation, the dynamic supervision analysis system of soil and water conservation was designed and conducted.[Methods] The system divides the minimum factor patch by multi-factor vector overlay analysis technology, and takes it as the supervision object. Through creating independent supervision task files for each supervision object, the task is assigned to the relevant responsible person in the region, and the task file circulation is used to promote and coordinate the implementation of specific supervision work of water administrative departments at all levels, so as to ensure all regulatory changes of task files information is transparently shared in the process.[Results] The experimental results of soil and water conservation monitoring stations in Jiangsu province show that the system takes districts and counties as the unit, it can integrate the monitoring and supervision data of three business scenarios in each district and county, and integrate the data results of different resolutions and frequencies in a hierarchical manner, so as to realize the whole process information sharing management of dynamic supervision of soil and water conservation; the minimum factor patch generated by overlay analysis can be used to realize the information sharing management of the whole process It can be implemented in the process of on-site supervision, and effectively drive the transfer of task files among users in different positions through user rights management.[Conculsions] The system improves the information management level of the comprehensive supervision of soil and water conservation of the local government in the three aspects, coordinates the task management of provincial, municipal and county-level regulatory departments, and improves the work efficiency of the comprehensive supervision.
2021 Vol. 19 (3): 110-119 [Abstract] ( 348 ) [HTML 1KB] [PDF 11015KB] ( 445 )
 
Forum
120 LI Xiaoge, ZHANG Ying
A measurement of sustainable development of eco-economic system in the sandy land of Yulin city, Shaanxi province based on emergy analysis
[Background] Eco-economy sustainable development is an important part of China's sustainable development. At present, research on the eco-economic sustainability of ecological fragile zone in semi-arid desert area is relatively weak. Yulin city is located in the middle section of the farming pastoral ecotone in northern China and vulnerable to ecological environment. The 42% of its northern area is Mu Us Sandy Land. Studying the sustainable development of its eco-economic system is of significance for promoting environmental economic governance and sustainable development in ecologically fragile areas.[Methods] Collecting the macroeconomic and social development data and meteorological data of Yulin city from 2008 to 2018, using the emergy analysis method, the original data was divided into 5 categories according to emergy elements:renewable resources, non-renewable resources, input flow, output flow, and waste flow. The emergy of different elements was calculated, the emergy analysis table was compiled, the eco-economic evaluation system was constructed, it included the comprehensive development index of social, economic and natural subsystems, and the eco-economic development and sustainability of Yulin city from 2008 to 2018 was evaluated.[Results] 1) In general, from 2008 to 2018, the total use of emergy in Yulin city increased from 1.97×1023 to 5.33×1023 sej, and the emergy of non-renewable resources accounted for 80.49%-85.20%, belonging to the economic mode of high energy consumption. 2) From the perspective of social subsystem, the emergy per person of Yulin city increased from 4.60×1012 to 1.22×1013 sej/m2, increasing by 2.65 times. Emergy intensity was constantly strengthening, but the population carrying capacity decreased from 232 000 to 137 000, the ecological environment was not enough to support population development. 3) From the perspective of economic subsystem, the emergy money ratio decreased from 1.36×1013 to 9.17×1012 sej/$.The speed of economic development and urbanization was accelerated, but the emergy load ratio decreased from 10.13 to 7.18, the emergy production efficiency reduced. 4) From the perspective of ecological subsystem, the energy self-support ratio reached over 85%, the environment load ratio increased from 11.92% to 20.53%, and the environmental pressure was increasing. The emergy index for sustainable development ESID dropped from 253.0 to 163.60.[Conclusions] The economic development of Yulin city mainly comes from the development and utilization of local non-renewable resources. The external output energy value is insufficient. In the long run, the energy utilization structure is unreasonable, the eco-economy system presents an unsustainable development trend, and the support capacity of system resources for economic development is constantly declining. Thus the sustainable ability of regional eco-economy can be improved from the aspects of regional industrial waste gas treatment, energy structure adjustment, external resource input, etc.
2021 Vol. 19 (3): 120-129 [Abstract] ( 339 ) [HTML 1KB] [PDF 1921KB] ( 327 )
 
Review
130 LIU Jing, LIU Zhilin, DING Yinping, JIAO Yuanmei, WANG Jinliang, YANG Yanfen, WU Changrun
Network atlas analysis of China's soil and water loss research progress in the past 20 years based on CiteSpace
[Background] This work aims to explore the law and frontier trend of soil and water loss research in China and promote the development of soil and water loss research.[Methods] This paper draws on the subject literature of the core journals above the "Water and Soil loss" in the CNKI Journal as a data source, uses CiteSpace as an analytical tool, and combines the thought of bibliometrics to draw a map of soil and water erosion research progress.[Results] 1) In the past 20 years, a group of professional researchers and research teams have emerged in the field of soil and water loss research in China. The research institutions are mainly universities and research institutes. 2) From 2000 to 2009, soil and water loss research is mainly the continuation and deepening of traditional, and paid attention to the combination of multiple technologies in research methods. At the same time, the research object and content are influenced by social demand and policy orientation. 3) During the 2010-2019 period it highlights the research orientation with sustainable development as the core. The research on soil and water loss during this period is divided into four parts:methodological research, engineering research, refined regional research and ecological civilization construction, showing the characteristics of wide-ranging and multi-level research.[Conclusions] In the past 20 years, the research on soil and water loss in China has been continuously developing, the research scale has been continuously refined, the research focuses on solving practical problems, and concurrently, the research direction is obviously policy-oriented to some extent. On future research more attentions should be paid to relationship between soil and water loss and ecosystem services and ecological civilization construction, soil and water loss and beautiful China under the context of climate change. Meanwhile, communication between teams and innovation of theories and methods should be strengthened.
2021 Vol. 19 (3): 130-138 [Abstract] ( 424 ) [HTML 1KB] [PDF 2040KB] ( 397 )
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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