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三峡支流消落带表层沉积物氮矿化动力学参数估算

刘丹 张帅 唐玉姣 尹静 谭兴伶 陈茜 于志国 林俊杰

农业环境科学学报2018,Vol.37Issue(4):766-773,8.
农业环境科学学报2018,Vol.37Issue(4):766-773,8.DOI:10.11654/jaes.2017-1482

三峡支流消落带表层沉积物氮矿化动力学参数估算

Parameter estimates of sediment nitrogen mineralization kinetics in the water level fluctuation zone of a Three Gorges Reservoir tributary

刘丹 1张帅 2唐玉姣 2尹静 2谭兴伶 2陈茜 2于志国 3林俊杰2

作者信息

  • 1. 重庆三峡职业学院农林科技系,重庆 万州404100
  • 2. 重庆三峡学院三峡库区水环境演变与污染防治重庆高校市级重点实验室,重庆 万州404155
  • 3. 南京信息工程大学水文气象学院,南京210044
  • 折叠

摘要

Abstract

To reveal the effect of drought-rewetting process on the nitrogen mineralization kinetics in the sediment of the water level fluctu-ation(WLF)zone, surface sediment samples were collected over various water level altitudes at the upper and downstream sections of the Pengxi River.The sediment nitrogen mineralization rate was evaluated with anaerobic incubation.The one-pool,two-pool,special,and effective accumulated temperature models(EATM)were applied to fit the data of nitrogen mineralization kinetics in sediments. The re-sult showed that total organic carbon(C),total nitrogen(N),organic matter(OM),clay,silt,and NH+4-N in the higher altitude were lower than that in the lower altitude,which is on the contrary to total phosphorus,sand,and NO-3-N.The one-pool model and special model were the optimal models for fitting nitrogen mineralization in sediments at low and high altitudes,respectively.The N mineralization rate constants (kd)were 0.17 d-1and 0.12 d-1,while the N mineralization potentials(fd)were 4.05% and 4.71% in the low and high altitude sediments,re-spectively.The fdwas negatively correlated with C,N,C/N ratio,OM,NH+4-N,and silt,and was positively correlated with NO-3-N and sand(P﹤0.05).The kdvalue had an opposite trend compared to the variation in fd.The model parameters of fdand kdwere successfully estimated by using the OM and C/N ratio.The current study revealed that nitrogen mineralization kinetics in sediment had a strong correlation with the water nitrogen content,and could thus be used to predict the contribution of nitrogen input into the WLF zone as an indicator of river eu-trophication.

关键词

三峡库区/氮矿化速率/水位波动/氮矿化模型/彭溪河流域

Key words

Three Gorges Reservoir area/nitrogen mineralization rate/water level fluctuation/nitrogen mineralization model/Pengxi River basin

分类

资源环境

引用本文复制引用

刘丹,张帅,唐玉姣,尹静,谭兴伶,陈茜,于志国,林俊杰..三峡支流消落带表层沉积物氮矿化动力学参数估算[J].农业环境科学学报,2018,37(4):766-773,8.

基金项目

重庆市教委科学技术研究项目(KJ1733441,KJ1601016) (KJ1733441,KJ1601016)

国家自然科学基金项目(31670467) (31670467)

教育部春晖计划项目(Z2015133) (Z2015133)

万州科技人才专项(2016-1) (2016-1)

三峡库区水环境演变与污染防治重庆高校市级重点实验室开放基金(WEPKL2016ZD-01,WEPKL2016ZZ-01)The Scientific and Technological Research Program of Chongqing Municipal Education Commission(KJ1733441,KJ1601016) (WEPKL2016ZD-01,WEPKL2016ZZ-01)

National Natural Science Foundation of China(31670467) (31670467)

Chunhui Project from Education Ministry of China(Z2015133) (Z2015133)

Talent Project of Wanzhou,China(2016-1) (2016-1)

Chongqing Municipal Key Laboratory of Institutions of Higher Education(WEPKL2016ZD-01,WEPKL2016ZZ-01) (WEPKL2016ZD-01,WEPKL2016ZZ-01)

农业环境科学学报

OA北大核心CSCDCSTPCD

1672-2043

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