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中国南方珠江口的营养物质特征与富营养化

The characteristics of nutrients and eutrophication in the Pearl River estuary, South China.

作者信息

Huang X P, Huang L M, Yue W Z

机构信息

South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 West Xingang Road, 510301, Guangzhou, China.

出版信息

Mar Pollut Bull. 2003;47(1-6):30-6. doi: 10.1016/S0025-326X(02)00474-5.

Abstract

In the spring of 1998, 24-h time series and synchronization of vertical profiles of NO(3)-N, NO(2)-N, NH(3)-N, PO(4)-P, chlorophyll a, suspended substance, salinity, temperature and other chemical parameters were taken at 10 stations in the Pearl River estuary in order to analyze the status and characteristics of nutrients and eutrophication. The results indicated that dissolved inorganic nitrogen (DIN) mainly came from the four river channels in the main estuary, and NO(3)-N was the main form of DIN in most area. The concentration of DIN was general above 0.30 mg l(-1) in the estuary, and more than 0.50 mgl(-1) in most part. Phosphate from four river channels was not the main sources, but land-based sources from the area near Shenzhen Bay or along the estuary were obvious, and other land-based sources outside the estuary brought by coastal current and flood tide current were also the main contributions. The concentration of phosphate was generally about 0.015 mg l(-1) except the area near Shenzhen Bay. The ratio of N:P was generally high, and it was higher in the north than in the south. The highest ratio was higher than 300, and the lowest one was over 30. The concentration of chlorophyll a was about 0.8-7.8 mg m(-3), and turbidity and phosphate may be the main two limiting factors for algal bloom in the estuary. The concentration of nutrients decreased slightly in the past decade, but still stayed at a high level. The nutrients mainly came from domestic sewage, industrial wastewater, agriculture fertilizer and marine culture in the Pearl River estuary.

摘要

1998年春季,在珠江口10个站位采集了24小时时间序列以及硝酸盐氮(NO(3)-N)、亚硝酸盐氮(NO(2)-N)、氨氮(NH(3)-N)、磷酸盐(PO(4)-P)、叶绿素a、悬浮物、盐度、温度等化学参数的垂直剖面数据,以分析营养盐状况及富营养化特征。结果表明,溶解无机氮(DIN)主要来自河口主河道的四条河流,且在大部分区域NO(3)-N是DIN的主要形态。河口区DIN浓度一般高于0.30 mg l(-1),大部分区域超过0.50 mgl(-1)。来自四条河流的磷酸盐并非主要来源,但深圳湾附近区域或沿河口的陆源明显,由沿岸流和涨潮流带来的河口外其他陆源也是主要贡献。除深圳湾附近区域外,磷酸盐浓度一般约为0.015 mg l(-1)。氮磷比普遍较高,北部高于南部。最高比值高于300,最低值超过30。叶绿素a浓度约为0.8 - 7.8 mg m(-3),浊度和磷酸盐可能是河口藻类爆发的主要两个限制因素。过去十年营养盐浓度略有下降,但仍处于较高水平。珠江口营养盐主要来自生活污水、工业废水、农业化肥和海水养殖。

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