• 中文核心期刊
  • 中国科技核心期刊
  • ISSN 1007-6336
  • CN 21-1168/X
SUN Zhen-hong, XU Guo-hui, YOU Qi, FANG Hong-ru. Release of nitrogen and phosphorus from sediment under liquefaction[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2016, 35(2): 203-208. DOI: 10.13634/j.cnki.mes.2016.02.008
Citation: SUN Zhen-hong, XU Guo-hui, YOU Qi, FANG Hong-ru. Release of nitrogen and phosphorus from sediment under liquefaction[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2016, 35(2): 203-208. DOI: 10.13634/j.cnki.mes.2016.02.008

Release of nitrogen and phosphorus from sediment under liquefaction

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  • Received Date: October 29, 2014
  • Revised Date: January 07, 2015
  • Sediments in lakes and coasts can release N and P into the overlying water due to static diffusion or resuspension, the value of which may be higher than that of static diffusion.Moreover, the resuspension under sediment liquefaction may have important impact on the concentration of N and P in water.In this paper, flume experiments were carried out to study the release of N and P at phase of consolidation(I), non-liquefaction(Ⅱ), and liquefaction phase(Ⅲ).The results showed that the concentrations of total phosphorus(TP), total dissolved phosphorus(TDP), total nitrogen(TN) and total dissolved nitrogen(TDN) were lowest at phase I, the concentration of TP at phase Ⅱ increased several times than those at phase I, the concentration of TDP at phase Ⅱ meanly increased by only 0.2 times than those at phase I; the concentration of TP and TDP increased most(up to 59 times and 25 times, respectively) at phase Ⅲ with 14 cm wave height.The concentration of TN and TDN at both phase Ⅱ and Ⅲ increased several times than those of phase I.
  • [1]
    李文霞,冯海艳,杨忠芳,等.水体富营养化与水体沉积物释放营养盐[J].地质通报,2006,25(5):602-608.[4]朱广伟,秦伯强,高光.风浪扰动引起大型浅水湖泊内源磷暴发性释放的直接证据[J].科学通报,2005,50(1):66-71.[7]李一平,逄勇,吕俊,等.水动力条件下底泥中氮磷释放通量[J].湖泊科学,2004,16(4):318-324.[8]朱广伟,秦伯强,张路,等.太湖底泥悬浮中营养盐释放的波浪水槽试验[J].湖泊科学,2005,17(1):61-68.[10]许国辉,孙永福,于月倩,等.黄河水下三角洲浅表土体的风暴液化问题[J].海洋地质与第四纪地质,2011,31(2):37-42.[12]魏复盛.水和废水监测分析方法(第四版)[M].北京:中国环境科学出版社,2002.[13]北京林业大学.土壤理化分析实验指导书[M].北京:北京林业大学出版社,2002.[14]宋新龙,王宇,汪灿.岩质边坡随机楔体稳定性分析的Monte-Carlo模拟[J].安全与环境工程,2012,19(1):112-116.[15]文威,孙学明,孙淑娟,等.海河底泥氮磷营养物静态释放模拟研究[J].农业环境科学学报,2008,27(1):295-300.[16]夏波,张庆河,蒋昌波,等.水体紊动作用下湖泊泥沙解吸释放磷的实验研究[J].泥沙研究,2014(1):74-80.[17]范成新,张路,秦伯强,等.风浪作用下太湖悬浮态颗粒物中磷的动态释放估算[J].中国科学(D辑:地球科学),2003,33(8):760-768.[18]梁文,张生,李畅游,等.污染水体沉积物营养盐释放过程[J].环境化学,2011,30(10):1718-1724.[19]李文红,陈英旭,孙建平.不同溶解氧水平对控制底泥向上覆水体释放污染物的影响研究[J].农业环境科学学报,2003,22(2):170-173.[20]刘红.长江河口泥沙混合和交换过程研究[D].上海:华东师范大学,2009.
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