岩石和小脑对土壤表面的影响对模拟结果的预测雪崩的影响

Oktaviani Putri Lestari, S. Utami, Christanti Agustina
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引用次数: 0

摘要

滑坡是印尼境内经常发生的自然灾害。2003 - 2018年滑坡总数为363起,主要由控制因素、触发因素或抑制因素引起。引起滑坡的两种因素(凋落物和岩石)之间的关系研究仍然很少。该研究于2020年9月至2021年3月在canar农业科技园和Jatimulyo实验站进行。模拟使用的是一个丙烯酸盒子(100厘米× 50厘米× 75厘米),在铝板上放置20厘米厚的土壤,以50°的坡度调整。降雨强度设定为70 mm h -1,使用可调水枪(作为降雨模拟器),电流为2.6安培旋转喷雾器a。测量的变量是滑坡持续时间和体积。然后使用非配对t检验分析获得的数据。显然,滑坡发生得越快,雪崩的体积就越大。在土壤质地、凋落物和地表岩石3个因素中,地表凋落物是影响滑坡持续时间和滑坡体积的最主要因素。当地表无凋落物时,两种土质类型的滑坡持续时间和滑坡体积差异较大。而当凋落物厚度为3 cm时,滑坡持续时间和滑坡体积在两种土质等级之间非常相似。在较小程度上,地表岩石的出现可以紧固和增加滑坡体积。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PENGARUH BATUAN DAN SERESAH PADA PERMUKAAN TANAH TERHADAP PENDUGAAN LONGSOR HASIL SIMULASI
Landslide is a natural disaster that often occurs in Indonesia. The total of landslides from 2003 to 2018 is 363, which were caused by controlling factors and triggering factors or restraining factors. The relation between two factors (litter and rock) that cause landslide is still rarely researched. This research was carried out from September 2020 to March 2021, in Agro Techno Park Cangar and Jatimulyo Experimental Station. A simulation used an acrylic box (100 cm x 50 cm x 75 cm), with soil 20 cm thick on an aluminium plate adjusted at a slope of 50°. Rainfall intensity was set at 70 mm hour-1, using an Adjustable Water Gun (as a rainfall simulator) with a current of 2.6 amperes rotation sprayer A. There were eight combination treatments consisting of three factors. The variables measured were landslide duration and volume. Data obtained were then analyzed using an unpaired t-test. Apparently, the faster the landslide occurs, the larger the avalanche volume. Among the three factors observed (soil texture, litter and rocks at the surface), surface litter was the most determining factor for landslide duration and volume. Landslide duration and volume were far different between the two soil textural classes when there was no litter at the soil surface. In contrast, if there was 3 cm litter, landslide duration and volume were quite similar between the two soil textural classes. To a small extent, the occurrence of the rocks at the soil surface may fasten and increase landslide volume.
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