Results 51 to 60 of about 2,594 (144)
River-groundwater transformation and ecological effects in the Tuwei River watershed [PDF]
The Tuwei River, an important tributary of the Yellow River, located in the eastern Jiziwan region exhibits a close hydraulic connection between atmospheric precipitation, groundwater, and river-lake water in the watershed. This connection influences the
Fan GAO +5 more
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Evaluation of freeze-thaw wind erosion and analysis of influencing factors on the Tibetan Plateau based on the improved RWEQ [PDF]
Freeze-thaw wind erosion refers to the process in which temperature fluctuations cause changes in the surface structure, significantly impacting on the formation of surface landform and soil properties. However, due to the particularity and complexity of
Fujun NIU +4 more
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Reduction theory and technical system of underground coal mining [PDF]
The coal mining changes the overburden boundary conditions and causes the redistribution of the in-situ stress and the deformation, movement, fracture of overburden rock.
Quansheng LI
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目的为揭示黄河上游乌兰布和沙漠段沿岸风沙入黄的物质输运特征与空间分异模式。方法选取沙漠-河流直接接触的典型过渡区,基于地表湿度梯度与沉积物粒度分异,将研究区域细分为边缘区(X1)、过渡区(X2)和近岸区(X3)3个子区域,系统分析表层沉积物粒度组成和输沙特征。结果边缘区以中细沙为主,平均粒径145.03 µm,风蚀作用强烈;过渡区中沙主导,平均粒径217.13 µm;近岸区以粉粒为主,平均粒径24.95 µm,水动力影响明显。各区域地表沉积物分选性差,偏度为极负偏-近对称-极负偏,峰态为尖窄-中等-尖窄。
李思瑶, 蒙仲举
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目前风沙危害是北京南郊地区面临的最为严重的生态环境问题之一.该区域的风蚀治理迫在眉睫。本文选择耕地、荒草地、流动沙地等永定河沙地典型的土地利用类型.通过定位实验观测与数学定量分析.进行沙地地表风沙活动的原理特征与风蚀防护措施的研究。研究结果认为:近地层风速随高度服从对数分布;下垫面性质不同导致对应的摩阻速度大小不同;不同利用类型下垫面对应的起沙风速明显不同;0~20cm高度范围内各层的输沙率百分含量随着高度的增加而减少,两者呈负指数函数;输沙率与风速呈正指数函数;风蚀地表组成物质明显粗化 ...
刘永兵 岳德鹏 王晓东
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Mining-affected water resources and ecological effects in ecologically fragile mining areas of western China [PDF]
The ecologically fragile mining area in the west is an important coal production base in China, and the current scale and intensity of coal mining has far exceeded its environmental carrying capacity, which is very likely to cause irreversible damage to ...
Liqiang YU +4 more
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由风蚀所导致的土壤物质再分配过程,决定了土地沙漠化的程度。根据半干旱干草原地区不同程度沙漠化土地土壤风蚀率的137Cs示踪结果,沙漠化各个阶段的土壤风蚀率指标为:潜在沙漠化土地以微弱堆积和微度风蚀为特征,风蚀率小于2000kg/(hm2·a);轻度沙漠化土地风蚀率介于2000~7000kg/(hm2·a)之间;中度沙漠化土地风蚀率大于7000kg/(hm2·a);重度沙漠化土地风蚀和堆积都很强烈,地表物质交换迅速,没有必要制定风蚀指标。
张春来 邹学勇 董光荣
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由于西北地区恶劣的气候环境,常年爆发强风沙天气,使高速列车车顶外绝缘常年暴露在强风沙环境中,引发绝缘放电导致事故频发。处于风沙环境下的气体放电特性与静态气体放电特性有较大差异,风沙环境下气流与沙尘对放电电离过程产生重要影响。文中以板—板电极所形成的均匀场为分析对象,考虑强风沙环境下气流速度、沙粒畸变电场和沙粒荷电捕获对放电过程所造成的影响,应用强化偶极子模型,推导了风沙条件下汤生电离系数的解析表达式。研究结果对于定量分析强风沙环境下气体放电特性具有理论参考价值。
史志鹏 +5 more
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[目的] 为明晰京津风沙源区生态系统服务时空格局特征及识别其冷热点,评估京津风沙源区实施生态工程后的生态效益及生态影响。[方法] 基于京津风沙源区2000—2017年的遥感、气象、土壤、土地利用等数据,利用CASA(carnegie-ames-stanford approach)模型、InVEST(integrated valuation of ecosystem services and trade offs)模型、RWEQ(revised wind erosion equation)模型和RUSLE(
常瑨予 +6 more
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采用室内分析和风洞模拟试验的方法,研究了不同风速下库布齐沙漠沙丘沙含水率对粗糙度、风速廓线和风沙流结构变化的影响。根据风洞实际动力情况,确定试验进口风速为6,8,10,12,14,16 m/s;除干沙外,人工配制了含水率为0.25%,0.5%,1.0%,1.5%,2.0%,2.5% 6组不同湿度的沙样,分别开展了风洞模拟试验。结果表明,地表粗糙度随着风速的增加而增大,但随湿度的增加整体呈减小趋势;试验所包含的湿度范围内,其风速廓线均随高度呈对数分布,随风速的增大,风速廓线的对数规律越好,风速梯度逐渐减小;
宗玉梅, 俎瑞平, 韩庆杰
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