河岸带表土层氮素非饱和入渗运移规律模拟

钱进; 王超; 王沛芳; 侯俊; 艾小榆

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河岸带表土层氮素非饱和入渗运移规律模拟

钱进, 王超, 王沛芳, 侯俊, 艾小榆

文章导航 > 水科学进展 > 2011 > 22(4): 568-573

钱进, 王超, 王沛芳, 侯俊, 艾小榆. 河岸带表土层氮素非饱和入渗运移规律模拟[J]. 水科学进展, 2011, 22(4): 568-573.

引用本文:

钱进, 王超, 王沛芳, 侯俊, 艾小榆. 河岸带表土层氮素非饱和入渗运移规律模拟[J]. 水科学进展, 2011, 22(4): 568-573.

QIAN Jin, WANG Chao, WANG Pei-fang, HOU Jun, AI Xiao-yu. Simulation of nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone[J]. Advances in Water Science, 2011, 22(4): 568-573.

Citation:

QIAN Jin, WANG Chao, WANG Pei-fang, HOU Jun, AI Xiao-yu. Simulation of nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone[J]. Advances in Water Science, 2011, 22(4): 568-573.

河岸带表土层氮素非饱和入渗运移规律模拟

钱进^1,2,
王超^1,2,,
王沛芳^1,2,
侯俊^1,2,
艾小榆²

1.
河海大学浅水湖泊综合治理与资源开发教育部重点实验室江苏南京 210098;
2.
河海大学环境学院江苏南京 210098

基金项目: 国家自然科学基金资助项目(50909035);江苏省自然科学基金攀登人才项目(BK2008041);中央高校基本科研业务费专项资金项目(2009B17214)

详细信息

作者简介:
钱进(1974- ),男,江苏海安人,讲师,博士,主要从事水污染控制与水生态修复研究.E-mail:hhuqj@hhu.edu.cn

通讯作者:
王超,E-mail:cwang@hhu.edu.cn

中图分类号: X143

Simulation of nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone

QIAN Jin^1,2,
WANG Chao^{1,2
,},
WANG Pei-fang^1,2,
HOU Jun^1,2,
AI Xiao-yu²

1.
Key Laboratory of Integrated Regulation and Resource Development of Shallow Lakes of MOE, Hohai University, Nanjing 210098, China;
2.
College of Environment, Hohai University, Nanjing 210098, China

Funds: The study is financially supported by the National Natural Science Foundation of China(No.50909035)

摘要: 自制土槽装置,室内模拟氮素在河岸带表土层中非饱和入渗的过程.通过观测土槽中不同点位渗流水体出流时间的先后顺序以及各点水体中TN、NH₄⁺-N浓度随入渗时间的变化,探讨氮素在河岸带表土层中非饱和入渗的运移规律.试验结果表明:在河岸带表土层非饱和入渗过程中,水分水平运移速度小于垂直运移速度,NH₄⁺-N的运移滞后于水分的运移;在土壤"干"-"湿"-"干"过程中,各点TN、NH₄⁺-N浓度值随时间先急剧增加再缓慢减少然后趋于稳定.另外,河岸带表土层对非饱和入渗氮素的截留效果较好,试验11 h时,在1.08m的坡长距离上,距土表面12 cm深度TN、NH₄⁺-N浓度比进水分别下降74.23%和68.02%.
- 河岸带 /
- 表土层 /
- 氮素 /
- 非饱和入渗 /
- 运移 /
- 土槽
Abstract: An experimental study was conducted in an indoor soil tank to examine to nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone.The timing of seepage flow from the tank and the seepage sequence at different sampling points were monitored.The variation of nitrogen concentrations(e.g.,total nitrogen TN and ammonia NH₄⁺-N)was also observed.Results show that the vertical velocity of percolation water is larger than the horizontal one during infiltration into the unsaturated topsoil layer of riparian zone.In the process from dry-towet and wet-to-dry,the TN and NH₄⁺-N concentrations first has a sharp increase and then gradually decrease until reaching a stable state.This is true for every monitoring point.In addition,the nitrogen retention capacity in the topsoil layer of riparian zone is high under unsaturated conditions.Along the 1.08 m long slope and 11 hours after the experiment began,the TN and NH₄⁺-N、oncentrations at points 12cm below the surface reduce by 74.23% and 68.02%,respectively.
- riparian zone /
- topsoil layer /
- nitrogen /
- unsaturated infiltration /
- transport /
- soil tank

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河岸带表土层氮素非饱和入渗运移规律模拟

1. 河海大学浅水湖泊综合治理与资源开发教育部重点实验室江苏南京 210098;

2. 河海大学环境学院江苏南京 210098

基金项目: 国家自然科学基金资助项目(50909035);江苏省自然科学基金攀登人才项目(BK2008041);中央高校基本科研业务费专项资金项目(2009B17214)

作者简介:
钱进(1974- ),男,江苏海安人,讲师,博士,主要从事水污染控制与水生态修复研究.E-mail:hhuqj@hhu.edu.cn

通讯作者: 王超,E-mail:cwang@hhu.edu.cn

收稿日期: 2010-06-21
修回日期: 2011-07-09
刊出日期: 2011-07-25

中图分类号: X143

关键词:

河岸带 /

表土层 /

氮素 /

非饱和入渗 /

运移 /

土槽

摘要: 自制土槽装置,室内模拟氮素在河岸带表土层中非饱和入渗的过程.通过观测土槽中不同点位渗流水体出流时间的先后顺序以及各点水体中TN、NH₄⁺-N浓度随入渗时间的变化,探讨氮素在河岸带表土层中非饱和入渗的运移规律.试验结果表明:在河岸带表土层非饱和入渗过程中,水分水平运移速度小于垂直运移速度,NH₄⁺-N的运移滞后于水分的运移;在土壤"干"-"湿"-"干"过程中,各点TN、NH₄⁺-N浓度值随时间先急剧增加再缓慢减少然后趋于稳定.另外,河岸带表土层对非饱和入渗氮素的截留效果较好,试验11 h时,在1.08m的坡长距离上,距土表面12 cm深度TN、NH₄⁺-N浓度比进水分别下降74.23%和68.02%.

English Abstract

Simulation of nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone

1. Key Laboratory of Integrated Regulation and Resource Development of Shallow Lakes of MOE, Hohai University, Nanjing 210098, China;

2. College of Environment, Hohai University, Nanjing 210098, China

Funds: The study is financially supported by the National Natural Science Foundation of China(No.50909035)

Received Date: 2010-06-21
Rev Recd Date: 2011-07-09
Publish Date: 2011-07-25

Keywords:

Abstract: An experimental study was conducted in an indoor soil tank to examine to nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone.The timing of seepage flow from the tank and the seepage sequence at different sampling points were monitored.The variation of nitrogen concentrations(e.g.,total nitrogen TN and ammonia NH₄⁺-N)was also observed.Results show that the vertical velocity of percolation water is larger than the horizontal one during infiltration into the unsaturated topsoil layer of riparian zone.In the process from dry-towet and wet-to-dry,the TN and NH₄⁺-N concentrations first has a sharp increase and then gradually decrease until reaching a stable state.This is true for every monitoring point.In addition,the nitrogen retention capacity in the topsoil layer of riparian zone is high under unsaturated conditions.Along the 1.08 m long slope and 11 hours after the experiment began,the TN and NH₄⁺-N、oncentrations at points 12cm below the surface reduce by 74.23% and 68.02%,respectively.

钱进, 王超, 王沛芳, 侯俊, 艾小榆. 河岸带表土层氮素非饱和入渗运移规律模拟[J]. 水科学进展, 2011, 22(4): 568-573.

引用本文:

钱进, 王超, 王沛芳, 侯俊, 艾小榆. 河岸带表土层氮素非饱和入渗运移规律模拟[J]. 水科学进展, 2011, 22(4): 568-573.

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河岸带表土层氮素非饱和入渗运移规律模拟

作者简介: 钱进(1974- ),男,江苏海安人,讲师,博士,主要从事水污染控制与水生态修复研究.E-mail:hhuqj@hhu.edu.cn

通讯作者: 王超,E-mail:cwang@hhu.edu.cn

Simulation of nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone

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河岸带表土层氮素非饱和入渗运移规律模拟

1. 河海大学浅水湖泊综合治理与资源开发教育部重点实验室 江苏南京 210098; 2. 河海大学环境学院 江苏南京 210098

作者简介: 钱进(1974- ),男,江苏海安人,讲师,博士,主要从事水污染控制与水生态修复研究.E-mail:hhuqj@hhu.edu.cn

通讯作者: 王超,E-mail:cwang@hhu.edu.cn

English Abstract

Simulation of nitrogen infiltration and movement through unsaturated soil in topsoil layer of riparian zone

1. Key Laboratory of Integrated Regulation and Resource Development of Shallow Lakes of MOE, Hohai University, Nanjing 210098, China; 2. College of Environment, Hohai University, Nanjing 210098, China

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作者简介:
钱进(1974- ),男,江苏海安人,讲师,博士,主要从事水污染控制与水生态修复研究.E-mail:hhuqj@hhu.edu.cn

通讯作者:
王超,E-mail:cwang@hhu.edu.cn

1. 河海大学浅水湖泊综合治理与资源开发教育部重点实验室江苏南京 210098;

2. 河海大学环境学院江苏南京 210098

作者简介:
钱进(1974- ),男,江苏海安人,讲师,博士,主要从事水污染控制与水生态修复研究.E-mail:hhuqj@hhu.edu.cn

1. Key Laboratory of Integrated Regulation and Resource Development of Shallow Lakes of MOE, Hohai University, Nanjing 210098, China;

2. College of Environment, Hohai University, Nanjing 210098, China