根系植物和凋落物对土壤宏观孔隙度、入渗速率和侵蚀的影响

Hanggari Sittadewi
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引用次数: 0

摘要

植物根系和树木生长产生的凋落物在雨水进入土壤(渗透)中具有重要的作用,作为未来的储水。植物根系和凋落物增加入渗速率的作用是由于增加了土壤的宏观孔隙度。根系分布在土壤剖面的各个层的存在将进一步增加土壤的有机质含量,使土壤松动,从而增加土壤的宏观孔隙度。此外,枯死的根系会形成空隙,可以被入渗的水填满;活跃的根系与土壤之间存在空隙,可以被入渗的水填满。高入渗率将减少过量径流水量,从而减少侵蚀的发生。
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EFFECTS OF ROOT PLANTS AND LITTER ON SOIL MACROPOROSITY, INFILTATION RATE AND EROSION
Plant roots and litter produced by tree that grow have an important role in the entry of rainwater into the soil (infiltration) as water storage in the future. The effects of plant roots and litter on increasing infiltration rate is due to increased soil macroporosity. The presence of roots that spread in various layers in the soil profile will further increase the organic matter content of the soil and loosen the soil thereby increasing soil macroporosity. In addition, dead roots will form empty spaces that can be filled by infiltration water, as well as active roots that have gaps between roots and soil that can be filled infiltration water. The high infiltration rate will reduce the amount of excessive runoff water so as to reduce the occurrence of erosion.
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EFFECTS OF ROOT PLANTS AND LITTER ON SOIL MACROPOROSITY, INFILTATION RATE AND EROSION MANGROVE ECOSYSTEM AND CLIMATE CHANGE MITIGATION: A LITERATURE REVIEW THE ROLE OF DISASTER-RESILIENT VILLAGES SUPPORTING TOURISM IN BADUNG DISTRICT ANALYSIS OF CAUSES OF SUBSIDENCE IN THE AREA NEAR UJUNGNEGORO STATION, BATANG REGENCY STUDI B-VALUE SEBAGAI ANALISIS SEISMISITAS BERDASARKAN DATA GEMPABUMI PERIODE 1914-2020 (STUDI KASUS : PROVINSI BENGKULU)
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