EFFECTS OF DRAINAGE DITCHES ON WATER TABLE LEVEL, SOIL CONDITIONS AND TREE GROWTH OF DEGRADED PEATLAND FORESTS IN WEST KALIMANTAN

IF 0.4 Q4 FORESTRY
D. Astiani, Burhanuddin Burhanuddin, L. Curran, M. Mujiman, R. Salim
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引用次数: 14

Abstract

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.
排水沟对西加里曼丹退化泥炭地森林地下水位、土壤条件和树木生长的影响
目前,由于森林砍伐和退化的加剧,热带泥炭地森林面临着相当大的压力。在加里曼丹,泥炭地森林的退化和砍伐主要是由工业伐木、主要通过将森林转变为农业用地和油棕榈种植园来扩大农业活动造成的。通过建立密集的排水系统,它可以在泥炭地引发野火。未经管理的排水沟将改变排水附近场地内的地下水位,包括周围泥炭地森林的地下水位。2007/2009年和2012/2015年,在西加里曼丹的库布拉亚泥炭地排水前后进行了地下水位评估。本文研究了排水沟对泥炭地地下水位的影响。结果表明,在泥炭地景观上建立排水沟将地下水位降低了3倍多,从~11.7厘米(SE=1.5,n=5)降低到~37.3厘米(SE=2.1厘米,n=26)。对地下水位的影响发生在7月至8月的干旱月份。地下水位的降低对土壤微气候、泥炭温度和泥炭含水量的影响最为严重。结果表明,随着排水系统的建立,泥炭地土地利用的变化对泥炭地地下水位产生了影响。在距离排水系统不到500米的区域,水位倾向于向排水特征降低。因此,泥炭地森林的恢复应通过管理景观水文(即地下水位)来启动,以恢复生态系统并保护剩余的泥炭沼泽森林。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
1.50
自引率
25.00%
发文量
18
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