湖泊和河流缓冲区宽度对印度尼西亚中爪哇湖泊Rawapening养分输出的影响:一个简单的模拟研究

Firda Maftukhakh, Hilmya Nada, N. Nugroho, N. Binti, Maulina Sofwan
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引用次数: 0

摘要

印度尼西亚的湖泊生态系统面临着严重的环境问题。其中一个问题是过量的植物营养物质,特别是氮和磷(P)引起的富营养化,水质退化和生物多样性丧失是富营养化的影响。印度尼西亚政府(GoI)发布了一项关于确定湖泊和河流缓冲区的规定,但尚未在实地全面实施。此外,与每个缓冲区宽度的影响相关的数据是不可用的。本研究旨在填补这一空白。模拟了湖泊和河流缓冲区宽度对Rawapening湖养分输出的影响。本研究使用了InVEST(环境服务与权衡综合评估)软件中的养分保留子模型来分析来自多个数据源的信息,包括数字高程模型(DEM)和土壤深度、年降雨量、土地覆盖/利用、流域/次流域边界和生物物理条件的测量。一些关于Rawapening湖富营养化的研究已经测量了富营养化的程度,但没有讨论缓冲区宽度的影响。因此,本研究包含了关于缓冲区宽度对减少养分输出有多大影响的最新数据。考虑了缓冲带宽度为30 m、90 m和150 m的5种情景,其中湖泊缓冲带宽度为30 m,河流缓冲带宽度为30 m。结果表明:湖泊缓冲带的最大养分输出减少量仅为氮的2.63%和磷的3.56%,而30 m的河流缓冲带宽度最大限度地减少了向Rawapening湖输出的氮的43.05%和磷的44.90%。30 m的湖流复合缓冲带宽度略微增加了养分输出的减少效果,分别为氮和磷的0.41%和0.56%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lake and Stream Buffer Zone Widths' Effects on Nutrient Export to Lake Rawapening, Central Java, Indonesia: A Simple Simulation Study
Lake ecosystems in Indonesia face serious environmental problems. One of those problems is eutrophication caused by excessive plant nutrients, particularly nitrogen (N) and phosphorus (P). Water quality degradation and biodiversity loss are the effects of eutrophication. The government of Indonesia (GoI) has issued a regulation on determining lake and stream buffer zones, but it has not been fully implemented in the field. Additionally, the data related to the effects of each buffer zone width is not available. This study aims to begin to fill this gap. It simulates the effect of lake and stream buffer zone widths on nutrient export to Rawapening Lake. The Nutrient Retention sub-model, which is part of InVEST (Integrated Valuation of Environmental Services and Tradeoffs) software, has been used for this research to analyse information from several data sources, including a Digital Elevation Model (DEM) and measurements of soil depth, annual rainfall, land cover/use, watershed/sub-watershed boundaries, and biophysical conditions. Several studies of eutrophication in Rawapening Lake have measured the magnitude of eutrophication but have not discussed the effects of buffer zone widths. Therefore, this study accommodates the updated data on how much effect of buffer zone widths on the reduction of nutrient export. Five scenarios of buffer zone width are considered:  30 m., 90 m., and 150 m, where the lake buffer zone widths and the stream buffer zone width are 30 m. The results indicated that the maximum nutrient export reduction of lake buffer zones was only 2.63% (for N) and 3.56% (for P). On the other hand, the 30 m stream buffer zone width reduced the nutrient export to Rawapening Lake by up to 43.05% for N and by 44.90% for P. A 30 m combined lake and stream buffer zone width slightly increases the nutrient export reduction effectiveness, i.e., 0.41% and 0.56% for N and P, respectively.
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