Results 41 to 50 of about 1,122 (146)
Meso and micro pore structure test of Jingyang shallow loess [PDF]
Rainfall and irrigation are the most common driving forces of geological disasters in loess areas. Generally, the infiltration depth is shallow and mainly controlled by microchannels.
Hengfei SUN +5 more
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Macro-micro Evolution Characteristic Function of Solidified Loess under the Effects of Dry-wet Cycles [PDF]
[Objective] To reveal the durability of solidified loess slope protection in long-term service. [Methods] Under the condition of dry-wet cycles, direct shear, permeability mechanical tests of solidified loess were carried out to study the evolution law ...
CHANG Zhou +6 more
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为明确秋耕对季节性冻融土壤热状况的调控作用,对比分析了翻耕(FG)、免耕(MG)、垄沟(LG)、翻耕活性炭覆盖(FH)和翻耕秸秆覆盖(FJ)5种处理对土壤温度、冻融循环以及土壤温度梯度等影响的差异。结果表明:与传统FG处理相比,MG、LG、FH、FJ处理均减弱了土壤温度与气温的相关性,降低了整个冻融期土壤温度的升、降温幅度和不同冻融阶段土壤温度昼夜变化的变异性程度,维持土壤温度序列稳定的能力FJ>FH>LG>MG。FG处理最先冻结和融化,其余处理延缓土壤冻结和融化速度的效果为FJ>FH>LG>MG ...
孙开, 王春霞, 蓝明菊, 梁飞
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为揭示季节性冻融区土壤侵蚀阻力的变化机制,确定影响土壤侵蚀阻力主控因子,通过室内冻融模拟、水槽冲刷和土壤抗剪试验,对黄绵土(SM粉质壤土)、风沙土(WS砂壤土)和黑土(KS黏壤土)侵蚀阻力影响因素进行研究。结果表明:(1)随着冻融循环次数增加,细沟可蚀性值逐渐升高,而临界剪切力降低。经历10次冻融循环后,SM粉质壤土、WS砂壤土和KS黏壤土的细沟可蚀性分别增加76%,63%,11%,临界剪切力分别减小37%,13%,91%。(2)细沟可蚀性随土壤抗剪强度、黏聚力和内摩擦角增大而减小 ...
卢超 +3 more
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Research on pore structural change of gravel soil under seepage erosion based on CT scanning [PDF]
As the main component of the landslide accumulation layer, gravel soil is affected by hydrodynamic factors; the change of internal seepage pressure leads to the loss of soil particles, resulting in the change of meso structure and mechanical properties ...
Da HUANG, Wenbo HUANG, Yikang GAO
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Temporal and Spatial Patterns of Wind Erosion Climate Indices and Their Responses to Atmospheric and Oceanic Circulation Patterns in the Chinese Mollisol Region over the Past 61 Years [PDF]
[Objective] A study on the spatial and temporal patterns of wind erosion climate indices and their responses to atmospheric and oceanic circulation patterns in the Chinese Mollisol region is of great significance for the early warning and prevention of ...
FU Jinxia +6 more
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[目的] 研究冻融作用对东北黑土区坡面土壤侵蚀的影响,可加深对黑土坡面侵蚀过程机理的认识,并为区域侵蚀治理提供重要科学依据。[方法] 以东北黑土区单一侵蚀营力驱动的融雪、风力和降雨侵蚀为对照,通过设计冻融-融雪、冻融-风力、冻融-降雨双侵蚀营力叠加的模拟试验,分析冻融作用对坡面融雪、风力和降雨侵蚀的影响。试验处理包括1次冻融作用、2个融雪径流量(1,2 L/min)、1个风速(12 m/s),1个降雨强度(100 mm/h)和1个坡度(3°)。[结果] (1)冻融作用显著增加坡面融雪、风力和降雨侵蚀量 ...
赵娅君 +7 more
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Preparation and response surface optimization of lightweight porous structures [PDF]
As a new type of building material structure, the porous structure still faces problems such as inaccurate optimal ratio and poor compatibility with plants, which affect its application.
Kai HE +7 more
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The Putuo Zongcheng Temple is the largest temple in the outer eight temples of “Chengde Mountain Resort and Outer Eight Temples”. It preserves a large number of stone cultural relics and has a high historical, artistic and scientific value.
Wu, Haijia
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通过对砒砂岩区西召沟小流域冻融风化侵蚀实测资料的分析,认为砒砂岩区冻融风化侵蚀主要发生在裸露沟谷坡面,其冻融风化侵蚀与砒砂岩的种类有关。与同种砒砂岩相比,种植沙棘7年后,支沟上、中、下游的坡面冻融风化侵蚀模数平均从11748t/km2降为3535t/km2,降低69.9%。单位长度沟沿线与沟角线和的冻融风化侵蚀量平均从0.0974m3/m降为0.004m3/m,降低95.9%。冻融风化侵蚀量占整个沟道总产沙量的百分比上游从76.1%降到52.6%,下游从6.4%升到13.2 ...
杨具瑞 毕慈芬 等
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