排序方式: 共有20条查询结果,搜索用时 203 毫秒
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西北地区黄土层中的脉管水规模较小,定位困难,视电阻率λ比值在水平及垂直方向均有很高的分辨率,能够准确地确定脉管水的空间位置。 相似文献
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西安地区黄土含水率变化特点 总被引:1,自引:1,他引:1
通过对西安地区黄土剖面的野外观察、颗粒分析和含水率的测定 ,系统地研究了黄土层含水率的变化特点 ,初步认识到在同一黄土剖面上 ,黄土含水率从上到下呈波动变化 ,其峰值位于古土壤层内 ,而波谷处于黄土层内 ,并呈波动增加的趋势。在具有结核层的黄土层中 ,其含水率从上部到下部呈由大变小再变大的趋势 ,其峰值位于结核层之上 ,CaCO3 结核层具有隔水作用 ;在古土壤层中 ,从上向下 ,其含水率呈由小变大再变小的规律 ,其峰值出现在古土壤的中、下部位 ,即粘土化最强的部位。土壤质地是决定含水率大小的重要因素 ,在包气带中 ,黄土含水率的变化与粘土颗粒含量具有明显的正相关关系。 相似文献
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介绍了在黄土层中施工70m以内仰斜排水孔用设备,钻具组合,钻进工艺参数、滤水管制作和下管工艺以及施工注意事项。 相似文献
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Holocene Yellow Silt Layers and the Paleoclimate Event of 8200 a B.P. in Lop Nur, Xinjiang, NW China
LIU Chenglin WANG Mili JIAO Pengcheng LI Shude CHEN YongzhiCollege of Environmental Sciences Peking University Yiheyuan Ro Haidian District Beijing Institute of Mineral Resources Chinese Academy of Geological Sciences Baiwanzhuang Ro Beijing 《《地质学报》英文版》2003,77(4):514-518
Many yellow silt layers have been identified in the Holocene sediments in the last lake of Lop Nur (playa), Xinjiang, northwestern China. Statistics of drill-hole cores have revealed more than one hundred layers, which exhibit regularity in time sequence. Study has further verified that these yellow silt layers were deposited through eolian processes. The time-frequency distribution diagram shows an obvious peak occurring at about 8200 a B.P., which is consistent with the dry, windy and cold climate event occurring at 8200 a in other places around the world. Therefore, this event is regarded as a response to the global climate change. 相似文献