印度尼西亚干旱早期信息的热带泥炭水分剖面

F. Marpaung, D. Fernando, S. Putiamini
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引用次数: 1

摘要

热带泥炭地是全球气候调节的主要因素之一。然而,由于土地清理和管理不善导致的反复发生的大规模火灾迅速摧毁了印度尼西亚的热带泥炭地。为了恢复这一生态系统,印尼政府采取了三项特别行动,即重新湿润、重新种植和社区赋权。这些活动需要泥炭水分的实时和实际信息。因此,我们调查了印度尼西亚南苏门答腊省Ogan Komering Ilir的土壤水分剖面。我们测量了5厘米、15厘米、25厘米和35厘米四个不同土层的土壤水分,以及两种类型的土地覆盖,即金合欢和油棕。结果表明,15 cm的变异小于其他土层。因此,印度尼西亚热带泥炭地15cm土层的土壤水分可以作为干旱的初步信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tropical Peat Moisture Profiles for Early Information of Drought in Indonesia
Tropical peatland is one of the main factors in global climate regulation. However, a repeatable large-scale fire as a result of land clearing and poor management practices rapidly devastates tropical peatlands in Indonesia. To restore this ecosystem, Indonesia government makes special actions by doing three activities, namely rewetting, replantation, and communal empowerment. These activities need real-time and actual information of peat moisture. Therefore, we investigated the soil moisture profile in Ogan Komering Ilir, South Sumatera Province, Indonesia. We measured soil moisture at four different soil layers, namely 5-cm, 15-cm, 25-cm, and 35-cm soil layer along with two types of land covers, namely acacia and oil palm. Results indicated that the variance of 15-cm was lower than other soil layers. Therefore, the soil moisture in the layer of 15-cm soil layer can be used as preliminary information of drought in tropical peatland, Indonesia.
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