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氮是水生生态系统中重要的营养元素，沉积物中氮的释放是上覆水中氮的重要来源和决定性因素[1]，对湖泊生态系统氮循环及由氮内源负荷引起的富营养化具有重要影响，而间隙水中各形态氮在沉积物-水界面氮循环系统中也扮演重要角色[2-3]。
沱江沉积物-间隙水中氮赋存形态及其环境地球化学
【摘 要】
：
氮是水生生态系统中重要的营养元素，沉积物中氮的释放是上覆水中氮的重要来源和决定性因素[1]，对湖泊生态系统氮循环及由氮内源负荷引起的富营养化具有重要影响，而间隙水中
【机 构】
：
天津市海洋资源与化学重点实验室,天津科技大学化工与材料学院,天津,300457天津市海洋资源与化学重点实验室,天津科技大学化工与材料学院,天津,300457;建筑与土木工程学院,成都大学,成都6101
【出 处】
：
中国化学会第六届全国热分析动力学与热动力学学术会议
【发表日期】
：
2017年11期
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