首页> 外文期刊>Geoderma: An International Journal of Soil Science >Exploration of the importance of physical properties of Indonesian peatlands to assess critical groundwater table depths, associated drought and fire hazard
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Exploration of the importance of physical properties of Indonesian peatlands to assess critical groundwater table depths, associated drought and fire hazard

机译:印度尼西亚泥炭地物理特性评估关键地下水表深度,相关干旱和火灾危害的重要性探讨

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Widespread degradation of Indonesian peatlands by deforestation and excessive drainage results into more frequent fires, particularly in El Nino years, which causes: (i) release of enormous amounts of peat soil carbon to the atmosphere, impacting climate, (ii) severe air pollution, affecting human health and air traffic, and (iii) decreased ecosystem services through loss of biodiversity. Groundwater table decline is the main driver of these negative processes and, therefore restoration of peatland hydrology is essential. Although groundwater table depth is critical to counteract peatland degradation, optimal depths are not generic for all peatlands, but depend on peat physical properties (i.e. water retention, unsaturated conductivity), which are related to the degree of peat humification (Fibric, Hemic, Sapric). Unfortunately only few of these peat physical properties are available while they are essential input data in hydrological models required to extend the usually short observed groundwater hydrographs. An experiment with the Soil-Water-Atmosphere-Plant model (SWAP) for two locations in Indonesian peatlands illustrates the impact of the degree of peat humification on physical properties and thereby on calculated groundwater table depth, hydrological drought and associated fires hazards. The Variable Threshold Method is applied to convert groundwater table depths into hydrological drought, and next the modified Keetch-Byram Drought Index (mKBDI) is used to assess wildfire hazard. Peat physical properties that reflect higher peat humification (Hemic and Sapric) result into lower water tables during dry periods, in particular during El Nino years, more severe hydrological drought, and an earlier and longer fire season. Using the limited available peat physical properties the importance is demonstrated of initiating a comprehensive programme to build a database of peat physical properties covering different environmental conditions in which tropical peatlands occur. Availability of such a database connected to a long-term monitoring programme, will support the ongoing rewetting, revegetation and revitalisation programme for Indonesian peatlands, which eventually will contribute to sustainable livelihoods for local people and reduce impact on the regional climate.
机译:森林砍伐和过度排水的印度尼西亚泥炭地的广泛退化导致更频繁的火灾,特别是在El Nino岁时,这导致:(i)释放到大气中的大量泥炭土壤碳,影响气候,(ii)严重的空气污染,影响人类健康和空中交通,(iii)通过丧失生物多样性减少生态系统服务。地下水表下降是这些负面过程的主要驱动因素,因此腐烂水文的恢复至关重要。虽然地下水表深度对抗泥土降解至关重要,但所有泥炭地都不是通用的最佳深度,但依赖于泥炭物理性质(即水保留,不饱和导电性),这与泥炭湿度(纤维,Hemic,Sapric相关)。 )。遗憾的是,只有很少的泥炭物理性质都可以使用,而它们是延长通常短的观测到地下水文文的水文模型中的基本输入数据。在印度尼西亚泥炭地区的两个地点进行土壤 - 水 - 大气 - 植物模型(交换)的实验说明了泥炭腐害程度对物理性质的影响,从而对计算的地下水位深度,水文干旱和相关火灾危害。将可变阈值方法应用于将地下水台深度转换成水文干旱,然后使用改进的Keetch-Byram干旱指数(MKBDI)来评估野火危险。泥炭物理性质反映泥浆湿度(Hemic和Sapric)在干燥期间导致较低的水表,特别是在El Nino岁期间,更严重的水文干旱,以及早期和更长的火季。使用有限的可用泥炭物理性质,证明了启动全面计划的重要性,以构建覆盖热带泥炭地发生的不同环境条件的泥炭物理性质数据库。这些数据库的可用性连接到长期监测计划,将支持印度尼西亚泥炭块的正在进行的重载,再训练和振兴计划,最终将为当地人民提供可持续的生计,并减少对区域气候的影响。

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