Results 51 to 60 of about 1,124 (149)
Effects of Tillage Disturbance on Slope Shape and Micro-topographic Features on Typical Sloping Cropland of Southwestern Alpine-canyon Area [PDF]
[Objective] The objective of this study was to investigate the effects of various tillage practices on on slope shape and micro-topographic features on typical sloping croplands of southwestern alpine-canyon area.
LIU Jingyi +8 more
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Remote sensing analysis of the changes in the ecotone of mangrove forests and Spartina alterniflora saltmarshes [PDF]
, 2017 红树林和盐沼是世界上重要的滨海湿地类型。在我国东南部沿海,互花米草盐沼和红树林之间的竞争成为一个重要的问题。为了研究红树林和互花米草盐沼之间的空; 间竞争规律,选取福建漳江口红树林国家级自然保护区为研究区域,收集了1988年至2014年27年间共15期覆盖该区域的Landsat影像和Goog; le Earth影像,采用最大似然分类法提取出红树林与互花米草盐沼的近30; a历史变化信息。历史遥感影像分析表明:1)红树林面积20世纪90年代增长速度最快,2004年以后增长速度变慢;2 ...
李屹, 李炎, 陈一宁
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Response of Runoff and Sediment Yield from Maize Slope Farmland in Karst Areas to Slope Gradient [PDF]
[Objective] To elucidate the responses of surface runoff, subsurface runoff, and underground runoff hydrological pathways to slope in maize sloping farmland in Karst regions.
DAI Quanhou +4 more
core +1 more source
Shuitu Baochi Xuebao, 2001 土壤剥蚀是指由侵蚀动力引起的土壤颗粒从土壤母质移动的过程。细沟剥蚀土粒随着细沟股流中含沙量的增加而减少 ,已有的一些侵蚀模型 (如 WEPP)均提到了这一点。用黄土高原一种典型的粉壤土 ,在 5种坡度、3种流量下进行了细沟侵蚀模拟试验。对试验结果进行了回归 ,分析了黄土高原斜坡及陡坡地、细沟股流剥蚀率随含沙量以及沟长变化的函数关系。这对细沟侵蚀动力过程的研究深入 ...
张晴雯 雷廷武 雷廷武 赵军
doaj +2 more sources
Shuitu Baochi Xuebao目的系统总结黄土高原重力侵蚀的研究进展，并提出未来需要解决的关键科学问题和研究方向，以期为流域重力侵蚀过程模型构建与黄土高原精准治理提供参考。方法综述重力侵蚀的观测与识别方法、动力与随机过程、水沙产输过程模拟及流域重力侵蚀模型构建等，特别是机载激光LiDAR技术的应用、基于土力学的边坡失稳模式和重力侵蚀的简化模型，分析现有研究中存在的观测方法功能单一、未考虑重力侵蚀随机性、缺乏重力侵蚀-水沙产输过程模拟方法等问题。结果目前，国内外在重力侵蚀单过程观测识别、重力侵蚀成因与经验评估等方面取得一定进展 ...
张攀, 韩志刚, 吴冰, 张羽飞
doaj
Characteristics and Drivers of Spatial and Temporal Soil Erosion in Anshun City, Karst Region [PDF]
[Objective] To explore the spatial and temporal evolution of soil erosion in Anshun City, southwest karst region, as well as the main controlling factors of soil erosion, and to master the soil erosion situation in the region, in order to help the ...
LI Yuan, LIU Ziqi, WU Wenxian
core +1 more source
Shuitu Baochi Xuebao, 2001 土壤剥蚀是指由侵蚀动力引起的土壤颗粒从土壤母质移动的过程，细沟剥蚀土粒随着细沟股流中含沙量的增加而减少，的一些侵蚀模型（如WEPP）均提到了这一点，用黄土高原一种典型的粉壤土，在5种坡度，3种流量下进行了细沟侵蚀模拟试验，对试验结果进行了回归，分析了黄土高原斜坡及陡坡地，细沟股流剥蚀率随含沙量以及沟长变化的函数关系，这对细沟侵蚀动力过程的研究深入，以及对侵蚀过程的预测预报提供了有力的参考依据。
张晴雯 雷廷武 等
doaj
, 1997 用数值方法模拟双锥、圆柱、椭球、圆锥和倒圆锥五类等质量异形铝粒子五种高宽比共25种粒子对半无限铝靶的超高速撞击侵蚀。撞击速度为4km/s。给出了抗深、坑径 ...
刘大有, 庄峰青
core
Bank collapse-landslide failure mechanism of typical reverse rock bank slope in Three Gorges Reservoir area [PDF]
At present, most of the reverse rock slope toppling instability failure is interpreted as a progressive overall instability failure controlled by dip angle and structural plane. However, the phenomenon of leading edge collapse is common in some reservoir
Bolin HUANG +4 more
core +1 more source
Shuitu Baochi Xuebao, 2017 以野外布设的径流小区为研究对象，采用模拟降雨方法研究随机条件下降雨侵蚀过程中泥沙有机碳含量及流失过程的动态变化规律。结果表明：（1）降雨侵蚀过程中泥沙有机碳含量随降雨的进行逐渐降低并趋于平稳，与坡面土壤有机碳含量相比显著增高（p＜0.01），有机碳在泥沙中明显富集，富集比最大值达1.780，泥沙中有机碳含量及富集比随侵蚀速率的增加明显减小且趋于稳定；（2）泥沙有机碳流失速率随降雨的进行先波动增大，达到最大值后又波动减小，最后逐渐趋于准稳定，整个过程呈单峰分布；（3 ...
任瑞雪, 杨明义, 王永吉
doaj