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地下水营养物质输入对印度尼西亚一个城市化热带河口系统的影响。

Groundwater nutrient inputs into an urbanized tropical estuary system in Indonesia.

机构信息

Leibniz Center for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany.

Leibniz Center for Tropical Marine Research (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany.

出版信息

Sci Total Environ. 2018 Jun 15;627:1066-1079. doi: 10.1016/j.scitotenv.2018.01.281. Epub 2018 Feb 6.

DOI:10.1016/j.scitotenv.2018.01.281
PMID:30857079
Abstract

Groundwater discharge is known to transport nutrients into estuaries at several locations around the world. However, few studies report groundwater-associated nutrient fluxes from tropical developing regions such as Southeast Asia, even though this area shows the strongest human modifications in the coastal zone worldwide. We investigated groundwater nutrient flux into two streams and estuaries (Awur and Sekumbu Bay) in the urban area of Jepara, Indonesia, and its relation with the land usage surrounding the estuaries. We found that average concentrations of NO, NH, and PO in Jepara's aquifer reached 145μM, 68μM, and 14μM, respectively, and our results indicate that these were mainly originated from untreated sewage, agriculture, and manure input. Approximately 2200tonNyear and 380tonPyear were removed in the soil and aquifer before the nutrients were discharged into the river. The total groundwater discharge into the river and estuary was estimated to 461×10md, or up to 42% of the river discharge. Discharge of groundwater-associated NO (72×10mold), NH (34×10mold), PO (5×10mold), and additional surface runoff may contribute to eutrophication and a decrease of nearshore surface water quality. Nutrient concentrations in groundwater, river, and coastal seawater in the Jepara region are similar to those found in major urban areas in Southeast Asia, e.g. Manila and Bangkok, even though Jepara has smaller size and population. Thus, our results indicate that medium populated cities with highly modified regional land use can contribute a significant amount of nutrient discharge in the coastal area and should be included in global assessments of nutrient budget calculation.

摘要

地下水排泄被认为在世界上许多地方将营养物质输送到河口。然而,很少有研究报告从东南亚等热带发展中地区的地下水相关营养物质通量,尽管该地区在全球沿海地区显示出最强的人为改造。我们调查了印度尼西亚日惹市两个溪流和河口(阿鲁和塞库布湾)的地下水营养物质通量及其与河口周围土地利用的关系。我们发现,日惹含水层中 NO、NH 和 PO 的平均浓度分别达到 145μM、68μM 和 14μM,我们的结果表明,这些主要来自未经处理的污水、农业和粪便输入。在这些营养物质排入河流之前,大约有 2200 吨氮/年和 380 吨磷/年被土壤和含水层去除。地下水排入河流和河口的总量估计为 461×10m/d,占河流流量的 42%。与地下水相关的 NO(72×10mold)、NH(34×10mold)、PO(5×10mold)的排放以及额外的地表径流可能导致富营养化和近岸地表水水质下降。日惹地区地下水、河流和近岸海水的营养物质浓度与东南亚主要城市如马尼拉和曼谷的浓度相似,尽管日惹的规模和人口较小。因此,我们的结果表明,人口众多、区域土地利用高度改造的中等城市可以为沿海地区的营养物质排放做出重大贡献,应纳入全球营养物质收支计算评估。

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