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Effects Of Drainage Ditches On Water Table Level, Soil Conditions And Tree Growth Of Degraded Peatland Forests In West Kalimantan

机译:加里曼丹西部排水沟对退化泥炭地森林地下水位,土壤条件和树木生长的影响

摘要

Currently, tropical peatland forests are under considerable pressure because of increasing deforestation and degradation of forests. In Kalimantan, degradation and deforestation of peatland forests are driven primarily by industrial logging, expansion of agricultural activities through primarily conversion of forests to agricultural land and oil palm plantations. By the establishment of intensive drainage, it can induce wildfires in peatland. Unmanaged drainage ditches will alter water table levels within the site adjacent to the drainage including to surrounding peatland forest. Water table assessments were conducted before and after peatland drainage on 2007/2009 and 2012/2015 in Kubu Raya, West Kalimantan. This paper studies the effect of drainage ditches into the peatland water table. Results show the establishment of drainage ditches on this peatland landscape lowered the water table by more than 3 times from ~11.7 cm (SE = 1.5, n = 5) to ~37.3 cm (SE = 2.1 cm, n = 26). The effect on the water table was in drier months of July-August. Lowering the water table level altered worst the soil micro climate, peat temperature and peat water content. The results indicate the land use changes in peatland with the establishment of drainage affects peatland water table currently. In the area of less than 500 m from the drainage, the water level tends to lower toward the drainage feature. Therefore, recovery of peatland forests should be initiated by managing the landscape hydrology (i.e. water table) to restore the ecosystem and to protect the remaining peat swamp forest.
机译:当前,由于越来越多的森林砍伐和森林退化,热带泥炭地森林承受着巨大的压力。在加里曼丹,泥炭地森林的退化和森林砍伐主要是由工业采伐,主要通过将森林转变为农田和油棕种植园来扩大农业活动。通过建立密集的排水系统,它可以在泥炭地引起野火。没有管理的排水沟将改变排水沟附近地点(包括周围的泥炭地森林)内的地下水位。在西加里曼丹的Kubu Raya,于2007/2009年和2012/2015年泥炭地排水前后对地下水位进行了评估。本文研究了排水沟对泥炭地地下水位的影响。结果表明,在该泥炭地景观上建立排水沟使地下水位降低了3倍以上,从〜11.7 cm(SE = 1.5,n = 5)降低到〜37.3 cm(SE = 2.1 cm,n = 26)。对地下水位的影响是在7月至8月的干旱月份。降低地下水位会改变土壤的微气候,泥炭温度和泥炭含水量。结果表明,随着排水的建立,泥炭地的土地利用变化目前影响泥炭地的地下水位。在距排水不到500 m的区域,水位趋于朝排水特征下降。因此,应通过管理景观水文(即地下水位)来恢复泥炭地森林,以恢复生态系统并保护剩余的泥炭沼泽森林。

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