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鄱阳湖沉积物中可迁移氮的分布及其对江湖关系变化的响应

[Distribution of transferable nitrogen in Poyang Lake sediments and its response to the variation of River-Lake relationship].

作者信息

Shen Hong-yan, Zhang Mian-mian, Ni Zhao-kui, Wang Sheng-rui

出版信息

Huan Jing Ke Xue. 2015 Jan;36(1):87-93.

Abstract

Amounts and distributions of total transferable nitrogen and different transferable nitrogen forms were studied in the sediments of Poyang Lake with different regimen, in order to reveal the influence of the water level change caused by the River-Lake relationship change on the potential release risks of nitrogen. The results showed that: (1) the contents of the total nitrogen (TN) were between 389 and 3865 mg x kg(-1), and the spatial distribution showed an overall downward trend in the "Five River", the "Hu Xin" and the northern regions; the contents of the transferable total nitrogen (TTN) were between 319.36 and 904.56 mg x kg(-1) and contributed 52% to the TN, and its spatial distribution trend was the same as that of TN. (2) The content of transferable nitrogen followed the order of SOEF-N approximately = SAEF-N > WAEF-N > IEF-N. (3) The dry period advanced and the low water level continued to decline as a result of the change in River-Lake relationship of the Poyang Lake, leading to the prolonged outcropped time of sediments and the increased area, causing the different contents of transferable nitrogen in the sediments at different elevations. The transferable nitrogen content of the sediments in the whole lake during the wet period was lower than that during the dry period. The content of transferable nitrogen followed the order of 12-13 m elevation sediment > 11-12 m elevation deposition material > 10-11 m elevation sediments. The higher the elevation, the longer the sediments were exposed, and the higher the transferable nitrogen content. (4) With the increase of elevation, all forms of N contents increased. The increase of IEF-N and SOEF-N contents as well as their percentages in total transferable nitrogen was relatively small, while the increase of WAEF-N and SAEF-N contents as well as their percentages in total transferable nitrogen was relatively large. If the river-lake relationship changes further, the elevation in the dry period will further decrease, which will lead to the enlarged area and prolonged exposure of sediments, resulting in increase of TN, transferable nitrogen, IEF-N and SOEF-N contents in the sediments. At the coming wet period of next year, the nitrogen release risk from sediments of Poyang Lake might increase.

摘要

为揭示江湖关系变化引起的水位变化对氮潜在释放风险的影响,研究了不同水情下鄱阳湖沉积物中总可转化氮及不同形态可转化氮的含量与分布。结果表明:(1)总氮(TN)含量在389~3865mg·kg⁻¹之间,空间分布在“五河”、“湖心”及北部地区总体呈下降趋势;可转化总氮(TTN)含量在319.36~904.56mg·kg⁻¹之间,占TN的52%,其空间分布趋势与TN相同。(2)可转化氮含量顺序为SOEF-N≈SAEF-N>WAEF-N>IEF-N。(3)鄱阳湖江湖关系变化导致枯水期提前且低水位持续下降,沉积物出露时间延长、面积增大,致使不同高程沉积物中可转化氮含量不同。全湖沉积物可转化氮含量在丰水期低于枯水期。可转化氮含量顺序为12 - 13m高程沉积物>11 - 12m高程沉积物>10 - 11m高程沉积物。高程越高,沉积物出露时间越长,可转化氮含量越高。(4)随高程增加,各形态氮含量均增加。IEF-N和SOEF-N含量及其在总可转化氮中的占比增加相对较小,而WAEF-N和SAEF-N含量及其在总可转化氮中的占比增加相对较大。若江湖关系进一步变化,枯水期高程将进一步降低,导致沉积物面积扩大、出露时间延长,沉积物中TN、可转化氮、IEF-N和SOEF-N含量增加。在明年即将到来的丰水期,鄱阳湖沉积物氮释放风险可能增加。

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