山体滑坡模拟:雨对土壤的强度影响,土壤有不同的纹理和有机物含量

Nur Fadillah Aunur Rofiq, S. Utami, Christanti Agustina
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引用次数: 0

摘要

自然因素和人为活动都可能导致山体滑坡。自然因素包括雨量大、多山或坡度陡的丘陵。可能导致山体滑坡的人为行为是土地改用和不当的土地管理。本研究旨在探讨降雨强度对不同质地和有机质含量土壤的影响。滑坡模拟研究是在巴西布拉维贾亚大学农学院农业科技园和实验田进行的。这项研究使用了一个丙烯酸盒子(尺寸为100厘米x 50厘米x 75厘米)和铝板作为基础,调整为50度的坡度。土壤质地(粉质和粘质)、降雨强度(70 mm h -1和120 mm h -1)和有机质施用量(不施和施有机质)3个因素组成8个处理组合。测量的变量是滑坡持续时间和体积。结果表明,滑坡物质的持续时间和体积受降雨强度的影响较大。与不施用有机质相比,在任何降雨强度下向土壤中添加有机质均可使滑坡持续时间和滑坡体积减少一半。在研究的三个因素(土壤质地、有机质施用和降雨强度)中,降雨强度似乎是滑坡持续时间和体积的最决定性因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SIMULASI PENDUGAAN LONGSOR: PENGARUH INTENSITAS HUJAN PADA TANAH DENGAN TEKSTUR DAN KANDUNGAN BAHAN ORGANIK YANG BERBEDA
Natural factors and human actions can cause landslides. Natural factors include high rainfall intensity and mountainous areas or hills with steep slopes. Human actions that can cause landslides are land conversion and inappropriate land management. This study aimed to explore the effect of rain intensity on soils with different textures and organic matter content. The landslide simulation study was conducted at the Agro Techno Park and Experimental Field, Faculty of Agriculture, Brawijaya University. This study used an acrylic box (size 100 cm x 50 cm x 75 cm) and aluminium plate as a base, which was adjusted to a slope of 50. There were eight treatment combinations consisting of three factors: soil texture (silty and clayey), rainfall intensity (70 mm hour-1 and 120 mm hour-1 ), and organic matter application (without and with organic matter application). The variables measured were landslide duration and volume. The results showed that the duration and volume of landslide materials are largerly influenced by rainfall intensity. Adding organic matter to the soil at any rainfall intensity may decrease landslide duration and volume by half compared to without organic matter application. Among the three factors examined (soil texture, organic matter application and rainfall intensity), rainfall intensity seems to be the most determining factor in landslide duration and volume.
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