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1.
黄土丘陵区坡面水土流失规律研究   总被引:2,自引:0,他引:2  
本文研究分析了三年大气降水,径流、泥沙资料,初步探求了坡度、降水和不同利用现状与水土流失的关系,并建立了降雨侵蚀力,坡度与坡面土壤侵蚀的数学模型,为该地区进行水蚀预报和防治工作提供了科学的依据。  相似文献   

2.
以青海省乐都县、互助县6条侵蚀沟为研究对象,收集了研究区域的降雨、地形地貌、植被、土壤等数据,系统分析了各因子与土壤侵蚀量的关系。结果表明,该研究区域年侵蚀厚度与年降雨总量的变化规律不明显,土壤容重、植被覆盖度和坡度三个因子的共同作用对侵蚀量有显著的影响。区域内各影响因子对土壤侵蚀影响的大小排序为:植被盖度坡度土壤容重土壤可蚀性降雨侵蚀力,再次说明退耕还林(还草)工程能够有效改善区域水土流失问题。  相似文献   

3.
董志塬核心区降雨侵蚀力时间分布及变化趋势   总被引:1,自引:0,他引:1  
利用董志塬中部西峰气象站1951-2011年逐日降雨量资料,采用日雨量侵蚀力模型、趋势系数和Mann Kendall突变检验法,分析董志塬核心区61 a来降雨侵蚀力的年内分布和年际变化特征。结果表明:① 董志塬核心区降雨侵蚀力在706.9~3 200.6 MJ•mm•hm-2•h-1•a-1,平均为1 634.7 MJ•mm•hm-2•h-1•a-1;其中7-9月降雨侵蚀力占全年的72.6%,冬季自1954年以来无侵蚀性降雨发生。② 61 a来年降雨侵蚀力变化趋势系数为0.005,春、秋两季有一定程度的下降,而夏季表现为上升趋势,但趋势均不显著。③ 突变检测表明,降雨侵蚀力波动幅度逐渐增加,表现为变率突变。其中,春季降雨侵蚀力标准差和变异系数在1972年前后增加了38.5%和47.8%;夏季4个变化阶段(1951-1969年、1970-1976年、1977-1984年和1985-2011年)降雨侵蚀力标准差和变异系数增加了36.3%和11.0%;秋季波动幅度略有减小趋势;年降雨侵蚀力标准差和变异系数在1952-1961年、1962-1974年、1975-1986年和1987-2011年4个阶段显著上升。尽管61 a来研究区降雨侵蚀力没有明显增加,但其变率突变将造成在波峰年对土壤更严重的侵蚀危害。  相似文献   

4.
不同土地利用方式对丘陵山区坡面侵蚀产沙量的影响   总被引:3,自引:0,他引:3  
选取安徽省霍山县大官山的典型研究区域,通过径流试验,分析了近20年6种典型土地利用方式的侵蚀产沙特性及影响因素.结果表明:不同土地利用方式对坡面侵蚀产沙量的影响依次是顺坡耕作区>标准小区>经济林区>牧草区>乔木用材林区>梯田小区.在不同土地利用方式下,防止土壤流失最有效的是梯田,而顺坡耕作区水土流失量最大.坡面侵蚀产沙量与降雨侵蚀力表现为幂函数关系,且相关性达到了极显著水平.  相似文献   

5.
甘肃省水土流失综合防治对策   总被引:1,自引:0,他引:1  
甘肃是西部水土流失较严重的省份之一 ,全省有水土流失面积 37.94× 1 0 4 km2 ,占全省土地面积的 83.5 %。黄河流域主要是水力侵蚀 ,长江流域为重力侵蚀 ,河西内陆流域以风力侵蚀为主。水土流失形成的自然因素为地质结构破碎、土壤质地疏松、降雨时空变率大、植被覆盖度差 ,是缓变因素。而不合理的水土资源开发 ,滥伐毁草过牧和工程建设等人类活动则是叠加在自然变化上的突变因素 ,加剧了水土流失。未来结合西部大开发的良好机遇 ,主要采取以小流域为单元的综合治理、因地制宜的实施退耕还林还草策略。  相似文献   

6.
TRMM数据应用于降雨量和降雨侵蚀力估算的适宜性研究   总被引:2,自引:0,他引:2  
USLE/RUSLE模型的模拟精度在很大程度上依赖于各个土壤侵蚀因子的准确估算,降雨侵蚀力因子R作为其最重要的因子之一,由于降雨实测资料不足而使其计算精度存在偏差.TRMM数据已被广泛应用于降雨数据估算,为解决这一难题提供了新的思路.文中基于2008 ~ 2009年TRMM 3B42数据集,采用已有计算方法,对我国2008 ~ 2009年降雨量和降雨侵蚀力进行了估算.并根据2008年实测降雨量以及已有研究成果对估算结果进行了对比分析和验证.结果表明:1)基于TRMM数据的降雨量估算值与实测数据具有较好的一致性,能够很好地反映降水变化过程,但与实测值之间仍存在一定偏差.2)2008年各月降雨量估算值与实测值之间的Nash-Sutcliffe系数E与均方根误差RMSE表现出相反的季节变化.3)多年平均R值与2008年和2009降雨侵蚀力估算值之间的相关系数分别为0.85和0.76,表现出较好的一致性.4)由于数据本身的局限性,TRMM数据对某些地区某些时段的降雨侵蚀力估计值普遍偏高.  相似文献   

7.
陕北地区煤炭资源开采过程中的生态破坏与对策   总被引:5,自引:2,他引:5  
陕北地区的煤炭资源开发给当地造成了严重的环境污染和生态破坏,对陕北地区煤炭开发给环境造成的大气污染、水污染、固体废弃物污染损失和给生态造成水源短缺、水土流失、植被破坏等损失分别进行经济计量,综合评价了陕北地区煤炭资源开发的生态环境价值损失。  相似文献   

8.
文中利用室内模拟降雨技术,通过不同覆沙方式和不同降雨强度的组合试验,对坡面侵蚀产沙特性进行了研究。得到结果:坡面初始产流时间基本随雨强的增大而提前。坡面覆沙后侵蚀量增多,且侵蚀量随雨强的增大而增大,半覆沙坡面的产沙量是全覆沙坡面的1.06~2.48倍。0.5、1.0mm/min雨强时半覆沙坡面产沙高于无覆沙坡面,1.5mm/min雨强时低于无覆沙坡面,而半覆沙坡面产沙则均高于全覆沙坡面。全覆沙破面含沙量受雨强影响较小,减沙效果较稳定。试验结果表明,坡面覆沙可以有效延迟初始产流时间;坡面覆沙后侵蚀程度增强,且随降雨强度的增大而增大,半覆沙坡面侵蚀程度高于全覆沙坡面;无覆沙坡面受降雨强度影响较大。文中为研究风水复合侵蚀提供了数据支撑,以期为揭示黄土坡面侵蚀发生机理和水土流失规律提供一些参考。  相似文献   

9.
残茬和秸秆覆盖对黄土坡耕地水土流失的影响   总被引:15,自引:1,他引:15  
通过田间试验与实验室模拟降雨试验,研究了残茬和秸杆覆盖对黄土坡耕地水土流失的影响。结果表明:坡耕地覆盖具有保水保土、减少土壤侵蚀的效果,而且随着覆盖量与覆盖年限的增加,效果更明显;在雨强为80、100mm/h模拟降雨条件下,与不覆盖相比,泥沙侵蚀率分别减少了97.8%与98.8%,溅蚀几乎没有,降雨入渗增加2.12倍和1.87倍,同时大幅度降低了侵蚀沉淀中氮和钾的浓度及土壤氮、钾总流失量。与基础土壤比较,侵蚀沉淀中氮钾具有养分富集作用。  相似文献   

10.
黄土丘陵沟壑区典型治理小流域水沙输移的尺度效应   总被引:1,自引:0,他引:1  
近年来,水土流失的尺度特征及尺度效应一直是土壤侵蚀研究的前沿。文中通过对黄土丘陵沟壑区第一副区不同空间尺度互为嵌套的小流域(5.97km~2的王茂沟小流域和70.1km~2韭园沟小流域)监测数据的分析,比较了流域治理措施实施后不同空间尺度小流域产流产沙过程及其对降雨事件的响应,揭示该流域淤地坝建设等措施对小流域泥沙输移特征的影响及其尺度效应。研究结果表明:两个尺度小流域径流对降雨响应过程均十分迅速,且退水后几乎没有基流,这同南方丘陵区小流域不同;王茂沟和韭园沟小流域径流量迅速增大,达到峰值后逐渐回退,大致在降雨停止6小时后完全消退;源头小流域(王茂沟)地表径流系数相较更大尺度小流域(韭园沟)略低,土壤流失量则相反;治理后的韭园沟小流域高含沙水流现象减少。重力侵蚀仍是源头区域发生高含沙径流的潜在影响因素,小流域尺度水土流失防治应重点治理源头区域。  相似文献   

11.
雨强和植被覆盖度对典型坡面产流产沙的影响   总被引:4,自引:0,他引:4  
应用先进的UGT水蚀测量仪,研究黄土高原祖厉河流域雨强和植被覆盖度对典型坡面产流产沙的影响。结果表明:黄土高原半干旱区间隔为15min的产流量、径流含沙量和产沙量与15min雨强具有相同的增减趋势,呈三次曲线关系y=b0+b1x+b2x2+b3x3。7种雨强条件下,人类扰动撂荒地的产流量、径流含沙量和产沙量均明显大于植被自然恢复的撂荒地,覆盖度20%的撂荒地是覆盖度35%撂荒地的平均径流系数的2.35倍,径流含沙量的4.48倍,产沙量的14.06倍。相对于受到扰动的撂荒地,植被自然恢复的撂荒地水土保持效益显著。  相似文献   

12.
黄土高原不同类型暴雨的降水侵蚀特征   总被引:27,自引:3,他引:24  
本文对黄土高原的三种类型暴雨的降水、侵蚀特征进行了统计分析,结果表明:A型暴雨的雨量多为10-30mm,历时一般为30-120min,最大60min降雨量占总雨量的85%-100%;B型暴雨的雨量一般为30-100mm,降雨历时多在3h-18h之间,最大60min降雨量占总雨量的30%-70%;C型暴雨的雨量一般为60-130mm,历时大于24h,最大60min降雨量占总雨量的8%-25%。三种类型暴雨的空间分布不均匀程度是A型大于B型,B型大于C型,且A型比B型、C型大得多。A型暴雨是引起土壤侵蚀的主要暴雨,其侵蚀性降雨发生的比例占侵蚀性降雨总次数的52.7%,其侵蚀量占总侵蚀量的64%。在坡面和沟道小流域,70%的极强烈侵蚀是由A型暴雨产生的。  相似文献   

13.
陇东黄土高原地表粗糙度对耕作土壤径流的影响   总被引:2,自引:0,他引:2  
用人工模拟降雨器,对陇东黄土高原不同地表粗糙度(RR)条件下翻耕土壤的径流和蓄水能力进行研究.以兰州大学庆阳黄土高原试验站为试验点,设3个处理:轻度(LR,RR=7.6 mm),中度(MR,RR=10.1 mm)和重度(HR,RR=21.0 mm)处理.结果表明:在66mm/h的降雨强度下,降雨开始的20min内,LR...  相似文献   

14.
浅析新构造运动对黄土高原水土流失的影响   总被引:7,自引:0,他引:7  
本文论述了新构造运动对黄土高原水土流失的影响。笔者认为,新构造运动对黄土高原水土流失起着控制作用。主要表现为:1.大范围的新构造运动导致黄土高原地区多暴雨,有利于地表土壤的侵蚀。2.新构造运动抬升,导致地区侵蚀基准面下降,新构造运动上升与沉降交汇处的地形突变带、断裂活动带、地震破碎带,地表土岩体不稳定,地表降水大量下渗,为重力和流水侵蚀创造了条件。3.新构造运动的形式、类型,制约地形的发育演化,控  相似文献   

15.
黄土高原侵蚀性降雨特征分析   总被引:12,自引:1,他引:12  
侵蚀性降雨是黄土高原地区剧烈土壤水蚀的原动力。利用黄土高原6个水土保持试验站20年以上的断点雨强资料和30年的气象站逐日降水观测资料,分析了侵蚀性降雨的发生频率、次降雨量、次降雨历时、次降雨侵蚀力以及降雨时程分布的统计特征:(1)黄土高原6个站侵蚀性降雨平均发生频率分别为7.0~13.4天/年,各站侵蚀性降雨的场雨量均值介于19.17~25.38mm,但变异性很大。各站次降水量、降雨历时和次降雨侵蚀力的频率分布都近似为指数分布。(2)根据本文设定的雨峰标准,黄土高原单峰降水占总降水次数的65%,双峰降水占30%,三峰降水占5%。峰值雨强的频率分布函数大致为Gamma分布中的一种,或者是偏正态分布,侵蚀性降水多为前锋型。上述结果可作为降水过程的随机模拟理论依据,也可以为全面深入研究土壤水蚀机理提供参考。  相似文献   

16.
As an important parameter in the soil erosion model, soil surface roughness(SSR) is used to quantitatively describe the micro-relief on agricultural land. SSR has been extensively studied both experimentally and theoretically; however, no studies have focused on understanding SSR on the Loess Plateau of China. This study investigated changes in SSR for three different tillage practices on the Loess Plateau of China and the effects of SSR on runoff and erosion yield during simulated rainfall. The tillage practices used were zero tillage(ZT), shallow hoeing(SH) and contour ploughing(CP). Two rainfall intensities were applied, and three stages of water erosion processes(splash erosion(I), sheet erosion(II) and rill erosion(III)) were analyzed for each rainfall intensity. The chain method was used to measure changes in SSR both initially and after each stage of rainfall. A splash board was used to measure the splash erosion at stage I. Runoff and sediment data were collected continuously at 2-min intervals during rainfall erosion stages II and III. We found that SSR of the tilled surfaces ranged from 1.0% to 21.9% under the three tillage practices, and the order of the initial SSR for the three treatments was ZT〈SH〈CP. For the ZT treatment, SSR increased slightly from stage I to III, whereas for the SH and CP treatments, SSR decreased by 44.5% and 61.5% after the three water erosion stages, respectively, and the greatest reduction in SSR occurred in stage I. Regression analysis showed that the changes in SSR with increasing cumulative rainfall could be described by a power function(R2〉0.49) for the ZT, SH and CP treatments. The runoff initiation time was longer in the SH and CP treatments than in the ZT treatment. There were no significant differences in the total runoff yields among the ZT, SH and CP treatments. Sediment loss was significantly smaller(P〈0.05) in the SH and CP treatments than in the ZT treatment.  相似文献   

17.
Soils(Leptosols or Epileptic Regosols)with lithic contact at a depth of 50 cm occupy almost 20%of the Brazilian semi-arid region.These lithic soils are susceptible to erosion due to faster saturation of water-holding capacity during rainfall,which accelerates the beginning of runoff.However,erosion traits of lithic soils in the semi-arid region of Brazil are less studied.The aim of this study was to characterize the soil and landscape attributes in areas with Neossolos Litólicos(Entisols)in the Caatinga biome to identify region of high susceptibility to erosion.Results showed that the soils were characterized by a sandy texture,soil structure with poor development and low content of organic carbon.These attributes increase susceptibility to erosion and reduce water storage capacity,especially in the states of Cearáand Sergipe.In these states,the content of rock fragments in the soil reaches 790 g/kg.High contents of silt and fine sand,high silt/clay ratio,predominance of Leptosols and strong rainfall erosivity were observed in Piauíand northwestern Ceará.A very high degree of water erosion was observed in the states of Pernambuco and Paraíba.Despite the low degree of erosion observed in the state of Bahia,it is highly susceptible to erosion due to the predominance of very shallow soils,rugged relief and high values of rainfall erosivity.Lower vulnerability was observed in the state of Alagoas because of its more smoothed relief,greater effective soil depth,thicker A horizon of soil and lower rainfall erosivity.In general,the characteristics that intensify the susceptibility to erosion in the Caatinga biome are those soil structures with poor development or without aggregation,low contents of organic carbon,high contents of silt and fine sand,high values of silt/clay ratio and rugged relief in some regions.This study collected information contributing to a better characterization of soils with lithic contact in the semi-arid region of Brazil.In addition,regions with a higher susceptibility to erosion were identified,revealing insights that could help develop strategies for environmental risk mitigation.  相似文献   

18.
分析农业部西北旱作营养与施肥科学观测站27年的降雨量演变资料,探讨这种演变过程对冬小麦产量及其它相关性状的影响.结果表明:陇东地区降雨分布与小麦生长期需水错位,随着气候变化,这种错位持续加深.降雨量演变对冬小麦品种的性状产生了不同方向的影响,有效穗数与最高茎数趋于减少、株高降低;穗粒数、千粒重趋于增加;出苗期推迟,抽穗期提前,快速生长、发育阶段和全生育期明显缩短.同时,降雨对陇东旱塬小麦产量的关键限制时期逐步从小麦营养生长前期向生殖生长期推移.  相似文献   

19.
HE Qian 《干旱区科学》2020,12(5):865-886
Soil erosion in the Three-River Headwaters Region (TRHR) of the Qinghai-Tibet Plateau in China has a significant impact on local economic development and ecological environment. Vegetation and precipitation are considered to be the main factors for the variation in soil erosion. However, it is a big challenge to analyze the impacts of precipitation and vegetation respectively as well as their combined effects on soil erosion from the pixel scale. To assess the influences of vegetation and precipitation on the variation of soil erosion from 2005 to 2015, we employed the Revised Universal Soil Loss Equation (RUSLE) model to evaluate soil erosion in the TRHR, and then developed a method using the Logarithmic Mean Divisia Index model (LMDI) which can exponentially decompose the influencing factors, to calculate the contribution values of the vegetation cover factor (C factor) and the rainfall erosivity factor (R factor) to the variation of soil erosion from the pixel scale. In general, soil erosion in the TRHR was alleviated from 2005 to 2015, of which about 54.95% of the area where soil erosion decreased was caused by the combined effects of the C factor and the R factor, and 41.31% was caused by the change in the R factor. There were relatively few areas with increased soil erosion modulus, of which 64.10% of the area where soil erosion increased was caused by the change in the C factor, and 23.88% was caused by the combined effects of the C factor and the R factor. Therefore, the combined effects of the C factor and the R factor were regarded as the main driving force for the decrease of soil erosion, while the C factor was the dominant factor for the increase of soil erosion. The area with decreased soil erosion caused by the C factor (12.10×103 km2) was larger than the area with increased soil erosion caused by the C factor (8.30×103 km2), which indicated that vegetation had a positive effect on soil erosion. This study generally put forward a new method for quantitative assessment of the impacts of the influencing factors on soil erosion, and also provided a scientific basis for the regional control of soil erosion.  相似文献   

20.
黄土高原土壤水分与植被生产力的关系   总被引:39,自引:15,他引:39  
土壤水分生态条件的恶化愈来愈成为黄土高原植被建设和生态环境建设的限制因素,我们在对黄土高原土壤水分生态因素分析的基础上,探讨了黄土高原土壤水分的季节性变化、土壤剖面水分变化、区域水分变异规律,分析了土壤水分与植被生产力间的相互关系,并提出了改善黄土高原土壤水分生态环境、提高植被生产力的调控技术。  相似文献   

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