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Field testing of irrigation effects on the stability of a cliff edge in loess, North-west China

机译:灌溉对黄土悬崖边缘稳定性的影响试验

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As it is not uncommon that irrigation has triggered landslides in the Chinese Loess Plateau, a full-scale field testing in a typical cracked plateau in Heifangtai, Gansu Province of China to simulate such phenomenon was conducted. In the study, piezometers were installed to measure the groundwater, and crackmeters as well as inclinometers were used to measure the slope movement. Water was pumped from the nearby source daily to simulate the irrigation process. There was a sharp increase of pore pressure in the undisturbed loess below the crack when the inclinometer registered considerable movement due to the inflow of water via the crack. Such increase in pore pressure also dissipated rapidly. Eventually, the irrigation water daylighted at the major cracks from the face of the plateau leading to local failures. The results show that cracks have significant effects on the flow of the irrigation water into the ground. The rapid rise in the local pore water pressure had reduced the stability of the slope.
机译:由于灌溉在黄土高原引发滑坡的情况并不少见,因此在中国甘肃省黑坊台一个典型的裂隙高原进行了全面的田间试验,以模拟这种现象。在这项研究中,安装了压力计来测量地下水,裂缝计和倾角仪用于测量坡度。每天从附近的水源抽水以模拟灌溉过程。当倾斜仪由于水通过裂缝流入而引起相当大的运动时,裂缝下方未受干扰的黄土中的孔隙压力急剧增加。孔隙压力的这种增加也迅速消散。最终,灌溉水在高原表面的主要裂隙处采光,导致局部破坏。结果表明,裂缝对灌溉水流入地下的影响很大。局部孔隙水压力的迅速上升降低了边坡的稳定性。

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