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1.
Huang Jinbai Wen Jiawei Hinokidani Osamu Yasuda Hiroshi 《Environmental Earth Sciences》2014,72(9):3623-3633
The objectives of this study were to examine the runoff characteristics and to estimate water budget at the wind–water erosion crisscross region on the Loess Plateau of China. A small catchment known as Liudaogou that has representative meteorological and hydrological conditions of the wind–water erosion crisscross region was chosen as the study location. A numerical model for rainfall-runoff was developed and verified; rainfall-runoff calculation for 5 years (2005–2009) was performed. The observed data and numerical result of the surface runoff were used for evaluating runoff characteristics and estimating the annual water budget. Runoff rate was proportional to average intensity of rain. Even though rainfall duration was for few minutes, surface runoff was generated by intensity of more than 2.6 mm × 5 min?1, when rainfall duration exceeded 10 h; surface runoff was generated by an intensity of 0.6 mm × 5 min?1, while annual runoff rate was 10–15 %. The unit area of 1 km2 was adopted as the index area for estimating annual water budget. Runoff, evapotranspiration, variation of water storage, and habitant water consumption accounted for 20.4, 75.6, 0, and 4 % of the total annual precipitation, respectively. Results of this study provide the basis for further research on hydrology, water resources, and sustainable water development and utilization at the wind–water erosion crisscross region on the northern Loess Plateau where annual water resources are relatively deficient. 相似文献
2.
Soil erosion is a serious environmental and production problem in China. In particular, natural conditions and human impact have made the Chinese Loess Plateau particularly prone to intense soil erosion area. To decrease the risk on environmental impacts, there is an increasing demand for sound, and readily applicable techniques for soil conservation planning in this area. This work aims at the assessment of soil erosion and its spatial distribution in hilly Loess Plateau watershed (northwestern China) with a surface area of approximately 416.31 km2. This study was conducted at the Caijiamiao watershed to determine the erosion hazard in the area and target locations for appropriate initiation of conservation measures using the revised universal soil loss equation (RUSLE). The erosion factors of RUSLE were collected and processed through a geographic information system (GIS)-based approach. The soil erosion parameters were evaluated in different ways: The R-factor map was developed from the rainfall data, the K-factor map was obtained from the soil map, the C-factor map was generated based on Landsat-5 Thematic Mapper image and spectral mixture analysis, and a digital elevation model with a spatial resolution of 25 m was derived from topographic map at the scale of 1:50,000 to develop the LS-factor map. Support practice P factor was from terraces that exist on slopes where crops are grown. By integrating the six-factor maps in GIS through pixel-based computing, the spatial distribution of soil loss in the study area was obtained by the RUSLE model. The results showed that spatial average soil erosion at the watershed was 78.78 ton ha?1 year?1 in 2002 and 70.58 ton ha?1 year?1 in 2010, while the estimated sediment yield was found to be 327.96 × 104 and 293.85 × 104 ton, respectively. Soil erosion is serious, respectively, from 15 to 35 of slope degree, elevation area from 1,126 to 1,395 m, in the particular area of soil and water loss prevention. As far as land use is concerned, soil losses are highest in barren land and those in waste grassland areas are second. The results of the study provide useful information for decision maker and planners to take appropriate land management measures in the area. It thus indicates the RUSLE–GIS model is a useful tool for evaluating and mapping soil erosion quantitatively and spatially at a river watershed scale on a cell basis in Chinese Loess Plateau and for planning of conservation practices. 相似文献
3.
Rainfall is considered as one of the paramount factors for slope failures in many regions around the world, particularly in tropical and subtropical regions. To study the effect of rainfall storm and its duration on the stability of slopes with a thin soft band layer, a 2D seepage numerical analysis and experimental investigation were implemented on an unsaturated model, consisting of clayey sand soils with a thin soft layer inclined to the horizontal level by 30° at a slope angle of 50°. It was subjected to intensive rainfall 20 mm/h for 8 h. Positive pore water pressures and horizontal earth pressures were monitored during the rainstorm using sensors distributed inside the experimental model. Both the experimental and numerical simulation results showed that the stability of the slope decreased during the time of the rainfall storm. Infiltration of rainwater resulted in reduction of soil shear strength, due to the loss occurring in soil suction after 1 h of rainstorm; the tension cracks appeared at the top of the slope and a certain displacement was observed in the sliding blocks. During the time of rainstorm, the infiltrated water flowed out from the slope through the weak interlayer near to the toe causing piping and local failure, so the formed cracks at the top of slope grew and expanded due to sliding of the failed soil blocks. Moreover, the ground water table rose and the positive pore water pressures increased, resulting in a reduction of effective stress, which is considered as a main factor in soil shear strength. A surface runoff was also present following the full saturation of the slope, leading to dragging the fine particles with water flow causing erosion. The combination of piping and erosion effects led to a quick local failure at the toe, as well as sliding of the failed blocks and spreading of the cracks. 相似文献
4.
Impact of rainfall intensity on the hydrological performance of erosion control geotextiles 总被引：1，自引：0，他引：1
The impact of erosion control geotextiles on the surface runoff from slopes is quite variable and depends strongly on site-specific conditions (soil characteristics, slope morphology, climate, etc.), as has been shown in several earlier studies. In addition, little is known about the proportion of runoff reduction that is caused by the geotextile and the proportion that is caused by soil characteristics. To shed more light on this issue, an experiment was carried out to test the impact of 500 g m?2 jute nets (J500) and 400 g m?2; 700 g m?2 coir nets (C400, C700) on the surface runoff from simulated rainfall of four different intensities (I 1 = 18.7; I 2 = 27.2; I 3 = 53.6; I 4 = 90.5 mm h?1). Data on runoff volume, peak discharge and time to peak discharge were collected from 40 simulated rainfall events. An impermeable “no-soil” subgrade was used to examine the impact of the geotextile on runoff without any influence of soil. All tested geotextiles significantly reduced runoff (volume, peak discharge) at all rainfall intensities, with the exception of C400 and C700 during simulated rainfall intensity I 4. J500 seemed to have the most effective runoff reduction performance at all rainfall intensities. In general, as the rainfall intensity increased, the effectiveness of the geotextiles decreased. Interesting behaviour was observed for J500 under simulated rainfall intensity I 4—the effectiveness of the geotextile increased with the duration of the rainfall. 相似文献
5.
利用野外径流小区动态监测和人工模拟降雨试验,阐明了草被和灌木的减流减沙效应,从力学层面揭示了坡面侵蚀产沙的过程机理。结果表明,与裸地相比,野外坡面草地和灌木地径流量分别减少28.1%~56.5%和85.7%~100%、产沙量分别减少84.9%~90.7%和98.5%~100%;在人工模拟降雨强度下,草地和灌木地径流量分别减少51.9%~90.9%和61.7%~80.6%、产沙量分别减少93.6%~99.2%和95.5%~99.2%;植被具有明显的增强土壤抗剪强度的作用,不同植被坡面抗剪强度与剪切面上的法向压力成正比,且符合库仑定律;不同下垫面条件下土壤黏聚力与坡面径流量和侵蚀产沙量呈显著的负相关关系,随着黏聚力的增大,径流量和侵蚀产沙量呈下降趋势;草地和灌木地坡面侵蚀临界径流切应力分别为裸地的2.64~3.16倍和2.44~3.18倍,建立了不同被覆坡面临界径流切应力与土壤抗剪强度和黏聚力的关系。研究结果对定量评价植被减蚀作用和深化土壤侵蚀力学过程有一定的参考意义。 相似文献
6.
为探明细沟形态演变对坡面产流产沙的互反馈作用,采用室内模拟降雨和三维地形扫描等手段对细沟形态演变中的水沙变化过程进行了研究。试验分析了黄土在不同雨强（66 mm/h、94 mm/h和127 mm/h）条件下,不同细沟发育阶段的水沙过程变化规律。结果表明,黄土细沟形态演变过程对产沙的影响较大,而对产流的影响较弱。径流量的变化过程主要取决于土体透水性、土壤的结皮作用以及产流方式,坡面产流量有先增大后减小最后趋于平稳的趋势;产沙量的变化过程与细沟发育进程有明显的对应关系,尤其是坡面地貌信息熵与产沙量和侵蚀速率的相关系数分别达到0.954和0.916,细沟的出现会加剧侵蚀,使含沙量明显增加;不同雨强下坡面产沙的变化规律基本相同,细沟沟网稳定后的产沙量与降雨强度呈正相关关系。 相似文献
7.
Assessment of soil erosion risk using SWAT model 总被引：3，自引：2，他引：1
Manel Mosbahi Sihem Benabdallah Mohamed Rached Boussema 《Arabian Journal of Geosciences》2013,6(10):4011-4019
Soil erosion is one of the most serious land degradation problems and the primary environmental issue in Mediterranean regions. Estimation of soil erosion loss in these regions is often difficult due to the complex interplay of many factors such as climate, land uses, topography, and human activities. The purpose of this study is to apply the Soil and Water Assessment Tool (SWAT) model to predict surface runoff generation patterns and soil erosion hazard and to prioritize most degraded sub-catchment in order to adopt the appropriate management intervention. The study area is the Sarrath river catchment (1,491 km2), north of Tunisia. Based on the estimated soil loss rates, the catchment was divided into four priority categories for conservation intervention. Results showed that a larger part of the watershed (90 %) fell under low and moderate soil erosion risk and only 10 % of the watershed was vulnerable to soil erosion with an estimated sediment loss exceeding 10 t?ha?1?year?1. Results indicated that spatial differences in erosion rates within the Sarrath catchment are mainly caused by differences in land cover type and gradient slope. Application of the SWAT model demonstrated that the model provides a useful tool to predict surface runoff and soil erosion hazard and can successfully be used for prioritization of vulnerable areas over semi-arid catchments. 相似文献
8.
Statistical analyses and controls of root-zone soil moisture in a large gully of the Loess Plateau 总被引：1，自引：0，他引：1
Yinguang Shi Pute Wu Xining Zhao Hongchen Li Jiawen Wang Baoqing Zhang 《Environmental Earth Sciences》2014,71(11):4801-4809
Soil moisture variability and controls are little known in large gullies of the Loess Plateau which represent complex topography with steep slopes. This study analyzed spatial–temporal variability of soil moisture at the 0–20, 20–40, 40–60, and 60–80 cm depths in a large gully of the Loess Plateau based on root-zone soil moisture measurements for 3 years (2009–2011). The result showed that mean soil moisture, standard deviation (SD), and coefficient of variation, were highly dependent on depth; the highest mean value was observed at the 20–40 cm depth, while the lowest one was at the 0–20 cm depth. The SD increased with mean soil moisture for various depths as soil moisture was relatively wet; however, a transition that SD decreased with mean soil moisture occurred when soil moisture was relatively dry. Positive correlations exist between moisture contents over different depths, and that the relationships of the neighboring layers are relatively high with R 2 from 0.70 to 0.76. Correlation analysis, principle component analysis, and stepwise multiple regression analysis showed that soil particle size distribution and topography (slope and elevation) were the main environmental factors controlling soil moisture variability in the large gully. 相似文献
9.
降雨诱发的浅层黄土泥流规模小、流速快、冲击力强、发育范围广、难以防御、致灾频率高,近两年造成了大量人员伤亡,急需开展其形成机制与强度的研究。黄土物质组成与水敏性、坡体形态对降雨入渗—积水的响应、黄土斜坡对降水入渗的力学响应机制、富水黄土粘滞性流动特性是制约浅层黄土泥流形成的四种主要因素,分析这四种因素的对浅层黄土泥流形成的制约作用需解决斜坡降雨入渗的水文过程、非饱和土的力学效应及水土耦合的机制等前沿问题。本文对影响泥流形成的各因素研究的最新进展进行了综述,同时讨论了研究中的核心问题,并提出了相应的对策与方案,认为可从三方面开展研究:(1)定量描述泥流体积扩容特征,建立浅层黄土泥流启动与流动模式;(2)分析泥流与原状黄土物质成分、组成结构差异,开展黄土非饱和增湿力学变形试验,监测0°~60°单面坡与坡肩平缓斜坡的降雨入渗过程,研究坡体形态对雨水汇聚、入渗及基质吸力变化的控制特征,揭示泥流流体运动过程中水土响应机制;(3)对浅层黄土泥流物理力学模型进行解析,讨论泥流流动能量转化特征,建立降雨诱发泥流灾害的强度计算模型,为降雨泥流灾害危险性定量计算提供理论支撑。 相似文献
10.
针对淮北地区水土流失问题,利用野外人工模拟降雨试验,分析了不同雨强(40mm/h、60mm/h和80mm/h)和坡度(5°、10°和15°)条件下砂姜黑土和黄潮土产流产沙差异。结果表明:砂姜黑土初始产流时间长,产流总量小。坡面出现细沟时,砂姜黑土初始含沙量随时间变化有减小趋势,最终趋于稳定,而黄潮土含沙量呈波动变化;60mm/h、80mm/h雨强10°坡砂姜黑土产沙总量大于黄潮土,其他情况黄潮土产沙总量大于砂姜黑土,黄潮土土壤侵蚀严重。砂姜黑土表面细沟发育密度大,主要在坡面中下部,为相互连通的树枝状结构,而黄潮土表面细沟发育密度小,形成沟壑。两种土壤产流总量、产沙总量与坡度、雨强分别呈多元线性函数、多元幂函数关系,雨强对坡面产流产沙总量的影响大于坡度。 相似文献
11.
Soil erosion is a serious global environmental problem which limits the survival and development of human beings. In our country, due to the special physical geography and socio-economic conditions, soil erosion intensity is great, which is particularly prominent in Loess Plateau region. Therefore, preventing and controlling soil erosion, as well as reducing soil erosion in Loess Plateau have become the key to solving environmental problems in the region. Soil erosion on Loess Plateau is serious, and grassland vegetation has good effects on soil and water conservation, which can improve ecological environment well. After the implementation of the project about returning farmland to grassland on Loess Plateau, the ecological benefits mainly focused on soil and water conservation benefits, soil improvement benefits, water conservation benefits and species diversity benefits, etc. Grassland vegetation has an irreplaceable role in the construction of the ecological environment on Loess Plateau. Therefore, the role of grassland in preventing soil erosion has received more and more attention. Scholars have done lots of research involved in the relationship between grassland coverage and soil erosion, impacts of grassland on hydrodynamic parameters, effects of grassland on soil properties, reduction effects of grassland on runoff and sediment, and soil erosion process on grassland slope. However, there is little research on erosion effect induced by grassland cover. This paper mainly pointed out the following questions: First, grassland cover is influenced by many factors, but the relationship with soil erosion from the dynamic mechanism is rarely discussed; Second, there is no well-developed theory of overland flow erosion at present, which limits the study of hydrodynamic parameters on grassland slope; Third, establishment of mathematical model between grassland cover and soil resistance can accelerate the quantitative analysis of grassland influence on erosion; Fourth, comprehensive analysis of influencing factors on water reduction and sediment reduction effect on grassland are insufficient; Fifth, there are not many mechanisms to analyze the erosion process of grassland slope by using the hydrodynamic characteristics of slope; sixth, research results on grassland-induced erosion are mainly focused on leading to soil dry layer and we should continue to strengthen in the future. This paper summarized the previous results, and supplemented some studies about erosion caused by grassland, then pointed out the existing problems in current research and the areas that need to be strengthened in the future, aiming at reducing soil erosion on the Loess Plateau. 相似文献
12.
Evaluation of soil loss change after Grain for Green Project in the Loss Plateau: a case study of Yulin,China 总被引：2，自引：0，他引：2
Soil erosion is one of the serious and urgent issues in the Loss Plateau of China. Chinese government has implemented Grain for Green Project to restore the ecological environment since 1999. In order to explore the spatiotemporal evolution of erosion and sediment yield before and after Grain for Green Project in the Loss Plateau, annual soil loss of Yulin from 2000 to 2013 is estimated by Chinese Water Erosion on Hillslope Prediction Model in conjunction with Remote Sensing and Geographic Information Systems. This model has the characteristics of a simple algorithm and can be applied to predict erosion in the Loss Plateau. The result shows that vegetation cover increased significantly after Grain for Green Project, and the annual average value of NDVI increased from 0.20 to 0.33. The spatiotemporal variations of soil erosion are largely related to rainfall erosion distribution, slope, and land use type. The overall soil erosion categories in the south region are higher than those of the northwest. Mid slopes and valleys are the major topographic contributors to soil erosion. With the growth of slope gradient, soil erosion significantly increased. The soil loss has a decreasing tendency after Grain for Green Project. Although the rainfall of 2002 and 2013 is similar, the soil loss decreased from 5192.86 to 3598.94 t/(km2 a), decreasing by 30.33%. It is also expressed that soil loss appears a reducing trend in the same degree of slope and elevation in 2002, 2007, and 2013. Under the simulation of the maximum and the minimum rainfall, soil erosion amount in 2013 decreased by 29.16 and 30.88%. The study proved that GFG has already achieved conservation of water and soil. The results indicate that the vegetation restoration as part of the Grain for Green Project on the Loss Plateau is effective. 相似文献
13.
为探究砾石对工程堆积体土壤侵蚀的影响与其作用机制,通过室内模拟降雨研究了连续降雨下不同砾石含量的重壤质堆积体水蚀过程。结果表明:①堆积体砾石含量增加,坡面产流历时延长,产流率线性减小,土壤剥蚀率降低;②连续降雨下,堆积体所含砾石主要通过对坡面产流历时、坡面产流率、砾石覆盖率的多重影响发挥减沙作用,主成分回归方程可表达多个变量与平均土壤剥蚀率的关系;③一定砾石含量下,堆积体坡面砾石覆盖率随表土的剥离而增大,导致土壤剥蚀率呈指数函数递减趋势,并与累积土壤侵蚀总量存在较好的函数关系。工程堆积体所含砾石对土壤侵蚀程度的削减可为生产建设项目下垫面水土保持治理提供重要参考。 相似文献
14.
Frequent occurrence of landslides in the Chinese Loess Plateau has been influenced by the changes of water conditions. This paper, based on in-situ water scouring experiments under various slope gradients, cross-sectional discharge shapes and flow quantities, analyzed the rill flow information characteristics on a loess slope and its driving factors for anti-scourability of the loess stratum. The results show that the critical erosion slope gradient for the loess stratum (Q3) is about 24° and the mean erosion rate under half-round cross-sectional discharge is smaller than that under rectangular discharge. The relationship between flow quantity and mean erosion rate is linear and is positively correlated. Mechanical subsurface erosion was the primary condition responsible for water scouring on loess slopes because of stronger runoff channels such as vertical joints and large amounts of macro void caused by plants and animals. Loess anti-scourability is a significant issue to advance the research for soil and water conservation in the Loess Plateau of China. 相似文献
15.
喀斯特裸坡土壤侵蚀模拟研究 总被引：4，自引：0，他引：4
文章通过人工模拟降雨试验,研究不同地下孔（裂）隙度、基岩裸露率和雨强对地表、地下产流、产沙的影响,其结果表明:（1）土壤侵蚀与地下孔（裂）隙度具有较高相关性,地表产流、产沙随地下孔（裂）隙度的增大而减小,而地下则相反;（2）坡面径流刚产生时,雨滴击溅和薄层水流冲刷,土壤细小颗粒堵塞其毛管空隙,渗漏率减小,而地表径流量增大,土壤团聚体被破坏、分散和迁移,降水与土壤渗漏率增大,地表径流量减小,雨滴击溅增强,如此循环,降水与土壤渗漏率呈波动性变化;总体而言,地表、地下悬移质均随降雨历时呈下降趋势,而地表推移质则相反,地表、地下产流量变幅较小,趋于平行;（3）地表产流、产沙量随基岩裸露率增大呈波动性变化,总体呈下降趋势;而地下产流、产沙量随基岩裸露率增大呈波动性变化,总体呈增大趋势;（4）在较小雨强30 mm/h时,地表只产生悬移质流失,没有产生推移质流失;地表、地下产流、产沙都是随雨强增大而增大;雨强由30 mm/h增大到150 mm/h,地表累积产流量为538.5 L,累积产沙量为2 393.81 g,地下累积产流量为207.8 L,累积产沙量为687.73 g,累积产沙量的递增速率比累积产流量的递增速率要大,地表产流、产沙的递增速率大于地下产流、产沙的递增速率;（5）各因子与土壤侵蚀间相关程度为:降雨历时>雨强>地下孔（裂）隙度>基岩裸露率。该实验有助于为喀斯特地区的水土流失研究、评价及制订石漠化治理措施提供理论依据。 相似文献
16.
Parameter estimation for a karst aquifer with unknown thickness using the genetic algorithm method 总被引：5，自引：2，他引：3
The combination of ecological fragility and agricultural activity in the loess hilly–gully regions of western China has received
broad environmental concerns. In this region, rainfall and soil moisture can fatally influence crop production under dry land
farming. In this study, field experiments were conducted, from March 2001 to September 2005, to demonstrate the variation
of soil moisture and fertilizer contents at different depths in slope and terraced lands, and to evaluate the ecological impacts
and economic benefits in the terraced land of Loess Plateau. The results of both field test and Grey model (GM) calculation
show that the terraced land, as compared to the sloping land, in the agricultural area of the Loess Plateau tends to store
and retain much water, promoting more favorable interactions between water and fertilizer. During the months from March to
June of the year with less rainfall, the water supply for crop growth is mainly derived from the deep storage of soil moisture
accumulated from July to September of the previous year. The field experiments indicate that the crop yield of the 3-year-old
terraced lands was 27% higher than that of the sloping lands with slopes greater than 10°, and that the crop yield can increase
by 27.07 to 52.78% in the following cultivation years. In particular, potato was found to be more drought-resistant than winter
wheat, thus it is more suitable for the arid and semi-arid Loess Plateau regions. 相似文献
17.
黄土高原地区的土壤侵蚀具有水力侵蚀和重力侵蚀相伴发生的特点,在大多数针对黄土高原的侵蚀模型研究中未考虑重力侵蚀的影响,使得模型的模拟精度较差。针对黄土高原的侵蚀特点,采用量化影响重力侵蚀发生的主要因素,确定重力侵蚀发生的具体沟道栅格单元的方法,从而考虑了重力侵蚀对产输沙过程的影响。所建立的分布式土壤侵蚀模型以逐网格汇流的水文模型为基础,采用逐网格侵蚀输沙的模拟方式,能够模拟上方来水来沙对侵蚀输沙的影响。经小理河流域实测资料验证,模型具有一定的计算精度。 相似文献
18.
Leila Gholami Abdulvahed Khaledi Darvishan Ataollah Kavian 《Arabian Journal of Geosciences》2016,9(19):729
The soil conditioner in processes of soil conservation is important especially in heavily eroded areas. Because in this study done in Educational and Research Forest Watershed of Tarbiat Modares University, north of Iran, the experiments created four treatments of control and different wood chips with rates of 0.5, 1, and 1.5 kg m?2, by rainfall simulation in rainfall intensity of 60 mm h?1, and plot scale of 1 m2 on changing ponding time, runoff coefficient, sediment concentration, and soil loss. The results showed that the average change ponding time in control treatment and wood chip treatments with rates of 0.5, 1, and 1.5 kg m?2 were 4.25, 7.48, 11.63, and 12.45 min. Also, the average change runoff coefficient in control treatment and wood chip treatments with rates of 0.5, 1, and 1.5 kg m?2 were 50.03, 26.27, 15.28, and 13.17 %. The results also indicated that the wood chips could decrease average soil loss with the rates of ?52.15, ?82.18, and ?89.35 % compared with control treatment for 0.5, 1, and 1.5 kg m?2 of wood chips, respectively. The one-way ANOVA results showed that the runoff coefficient, sediment concentration, and soil loss decreased with increasing wood chip amount, and the effect of conservation treatment was significant on study variables (R 2 = 0.99). But, the ponding time increased with increasing wood chip amount, and this effect was significant on study variables (R 2 = 0.99). 相似文献
19.
采用多坡段组合模型、人工模拟降雨实验研究了土壤侵蚀链垂直带水沙流空间分布变化特征。结果表明:愈向下坡方向的坡段产流量愈大,单位面积、单位时间的产流量按坡段排列为:谷坡>梁峁坡下部>梁峁坡中部>梁峁坡上部。雨强为29.7mm/h时,坡面上没有沟蚀发育;雨强为60.5mm/h时,细沟主要分布在梁峁坡下部和谷坡处;雨强为90 2mm/h时,各种侵蚀形态在坡面均有较好发育,细沟的出现部位一直伸展到梁峁坡中部和上部之间。由于上坡来水来沙的作用,梁峁坡的产沙量增大了20.2%～63.5%,谷坡的产沙量增大了42.9%～74.5%。 相似文献
20.
为研究黄土丘陵沟壑区多种因素对撂荒草地入渗特征的影响,采用野外自然降雨观测法,研究不同降雨特征（降雨量、平均雨强、降雨历时和最大30 min雨强（I30））、土壤前期含水量、坡长（10 m、20 m、30 m、40 m和50 m）和植被盖度条件下土壤入渗特征差异,通过灰色关联度法判断影响撂荒草地入渗特征的主导因子。结果表明:①入渗量随降雨量、降雨历时和I30增加而增大（R2>0.55,P < 0.01）;入渗补给系数随降雨量、I30和平均雨强增大而减小（R2>0.12,P < 0.05）;平均入渗率随降雨强度、I30增加而递增（R2>0.53,P < 0.01）。②入渗量和平均入渗率随前期含水量增加而减少,入渗补给系数随之增加而增大（R2>0.13,P < 0.05）。③入渗量、入渗补给系数和平均入渗率总体随坡长增加而增大（R2>0.56,P < 0.01）,但在坡长30 m和40 m之间存在临界坡长。④在入渗效率较高的情况下,植被对土壤入渗的影响并不显著,降雨特征和坡长成为主导因子。 相似文献