[泥中的滑梯]底泥氮、磷和有机质含量竖向分布规律讲义.pdf
中国自然环境自然科学2010,30(4):493--498 China Environmental Science
西湖红树林气网氮、磷和盐份浓度壁面原产规律性
陈如海1,詹良通P,王震敏1,胡洪志2(1.江苏大学优柔寡断土与自然环境removal中华人民共和国教育部重点项目生物医学,江苏苏州310058;
2.苏州市林水局。江苏苏州310014)
全文:借助托盘的热量计从西湖红树林截叶已连续完备的气网待测,对相同广度气网中总氮fiN)、总磷rrP)和盐份(OM)浓度展开测试;通过
TN、TP、OM在海床气网、气网裂隙水和上覆地下水底浓度变动的预测结论,并借助无机成分股法对该红树林气网的自然环境污染某种程度展开了赞扬嚣果
说明,该红树林60era广度以上的气网为中度二中度自然环境污染。归属于特异性层;埋深小于60em的气网杜勒旺勒沙托县自然环境污染或是自然环境污染较重。归属于相较平衡层;TN、TP、
OM在垂向下的变动呈明显有关亲密关系.TN、TP在气网裂隙水底的浓度明显低于在上覆地下水底的浓度;由于存有径向,气网裂隙水底的
氮、磷或其他无机自然环境氮氧化物会释放出来到上覆地下水底去,只实行换水处理难以根除红树林地下水水污染的问题.对做为内自然环境氮氧化物的气网,疏濬应是一
种更有效率的环境治理举措,60cm特异性层广度可做为该红树林疏濬参照广度.
关键字:气网水污染;总氮;总磷;盐份;裂隙水:红树林
中图科同盘属:X142 历史文献N53SI241SV:A 该文序号:1000-6923(2010)04-0493-06
Contents of nitrogen,phosphorus and organic materials in sediments and theirs dbtribufion along depth at Xixi
Wetland.CHEN Ru-hail,ZHAN Liang-tong,CHEN Yun-minl,HU Hong-zhi2(1.Key Laboratory of Soft Soils and
Geoenvironmental Engineering,Ministry of Education,Zhejiang University,Hangzhou 3 1 0058,China:2.Hangzhou
Municipal Bureau ofForestry and Water Resource,Hangzhou 310014,China).China EnvironmentalScience,2010,30(4):
493--498
Abstract:A special sampler was made to take continous specimens of sediment(up to 2m long)from X议i Wetland.T11e
contents of total nitrogen(TN),total phosphorous(TP)and organic matter(OM)were measured on the sediment
specimens taken from different depths,and their distributions along depth in this wetland were determined.
Concentrations of TN,TP and OM in the pore-water of sediments and the upper water body were also measured.On the
base of the measurements,the eutrophication pollution degree in the sediments Was evaluated by using the organic index
method.It Was found that the active zone of pollution was extended to a depth of 60cm below the river bed.Sediments in
the active zone were slightly-moderately polluted,and nO pollution wag observed at the depth greater than 60cm(i.e.,
relatively stable Zone).The distributions of TN,TP and OM along depth showed a consistent trend.The amounts of TN
and TP in the pore water of shallow sediments wcrc found to be much more t