Water-level alterations modified nitrogen cycling across sediment-water interface in the Three Gorges Reservoir

被引:32
作者
Yu, Juhua [1 ]
Zhang, Yushu [1 ]
Zhong, Jicheng [2 ]
Ding, Hong [1 ]
Zheng, Xiangzhou [1 ]
Wang, Zhiyuan [3 ]
Zhang, Yinlong [4 ]
机构
[1] Fujian Acad Agr Sci, Inst Soil & Fertilizer, Fuzhou 350013, Fujian, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China
[3] Nanjing Hydraul Res Inst, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing 210029, Jiangsu, Peoples R China
[4] Nanjing Forestry Univ, Coinnovat Ctr Sustainable Forestry Southern China, Nanjing 210037, Jiangsu, Peoples R China
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Nitrogen cycle; Water-level regimes; Sediment-water interface; Reservoir; LAKE TAIHU; EUTROPHIC LAKE; HYPORHEIC ZONE; N2O EMISSIONS; OXIDE N2O; RIVER; PHOSPHORUS; NUTRIENT; RELEASE; DENITRIFICATION;
D O I
10.1007/s11356-019-06656-z
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Water-level regime alteration-associated redox fluctuation plays a primary role in governing exchange and transformation of nitrogen (N) in water-level fluctuation zones (WLFZs), while few understanding of how hydrological regimes under reservoir operation affected N cycling across the sediment-water interface (SWI), giving rise to uncertainties in reservoir N nutrient management. Batch microcosm simulation experiments with intact sediment cores from WLFZs of the Three Gorges Reservoir (TGR) were conducted for 24 days to identify holistic flooding-drying process mechanism on N-cycling patterns. Our results showed a distinct transition of N-cycling mode across the SWI, shifting from biological denitrogen loss dominated in initial period of flooding to enhance endogenous N retention. A dramatic source-sink switch of nitrous oxide (N2O) occurred in the first 1.5 days during the flooding period. However, combined accelerating migration of NH4+-N from sediment to overlying water, and subsequently enhanced transformation of NH4+-N to NO3--N formed from flooding to drying rotation, thereby increasing N loading to overlying water. The reason for this investigation could be attributed to intensive N loss through coupled nitrification and denitrification in oxic-anoxic microenvironments after flooding. With oxygen replenishment from atmosphere during drying phase, persistent ammonification of organic N in sediments provided sufficient source of NH4+-N for the formation of NO3--N fraction in a more oxic overlying water. Therefore, water-level regime alteration by reservoir operation was capable of weakening N removal from water body and lengthening internal N turnover time across redox-variable SWI. These findings elucidate new understanding of holistic hydrological regime mechanisms on N cycling across SWI and provide insight to biogenic N nutrient management for improving the green credentials of hydroelectric reservoir.
引用
收藏
页码:25886 / 25898
页数:13
相关论文
共 49 条
[1]  
Baldwin DS, 2000, REGUL RIVER, V16, P457, DOI 10.1002/1099-1646(200009/10)16:5<457::AID-RRR597>3.0.CO
[2]  
2-B
[3]   The water-level fluctuation zone of Three Gorges Reservoir A unique geomorphological unit [J].
Bao, Yuhai ;
Gao, Peng ;
He, Xiubin .
EARTH-SCIENCE REVIEWS, 2015, 150 :14-24
[4]   Nitrous oxide emission from denitrification in stream and river networks [J].
Beaulieu, Jake J. ;
Tank, Jennifer L. ;
Hamilton, Stephen K. ;
Wollheim, Wilfred M. ;
Hall, Robert O., Jr. ;
Mulholland, Patrick J. ;
Peterson, Bruce J. ;
Ashkenas, Linda R. ;
Cooper, Lee W. ;
Dahm, Clifford N. ;
Dodds, Walter K. ;
Grimm, Nancy B. ;
Johnson, Sherri L. ;
McDowell, William H. ;
Poole, Geoffrey C. ;
Valett, H. Maurice ;
Arango, Clay P. ;
Bernot, Melody J. ;
Burgin, Amy J. ;
Crenshaw, Chelsea L. ;
Helton, Ashley M. ;
Johnson, Laura T. ;
O'Brien, Jonathan M. ;
Potter, Jody D. ;
Sheibley, Richard W. ;
Sobota, Daniel J. ;
Thomas, Suzanne M. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2011, 108 (01) :214-219
[5]   River basin nutrient delivery to the coastal sea: Assessing its potential to sustain new production of non-siliceous algae [J].
Billen, Gilles ;
Garnier, Josette .
MARINE CHEMISTRY, 2007, 106 (1-2) :148-160
[6]   Diurnal fluctuations of dissolved nitrous oxide (N2O) concentrations and estimates of N2O emissions from a spring-fed river:: implications for IPCC methodology [J].
Clough, Tim J. ;
Buckthought, Laura E. ;
Kelliher, Francis M. ;
Sherlock, Robert R. .
GLOBAL CHANGE BIOLOGY, 2007, 13 (05) :1016-1027
[7]   Quantification of ammonia-oxidizing bacteria and factors controlling nitrification in salt marsh sediments [J].
Dollhopf, SL ;
Hyun, JH ;
Smith, AC ;
Adams, HJ ;
O'Brien, S ;
Kostka, JE .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2005, 71 (01) :240-246
[8]   COMMENTARY: Greenhouse-gas emissions from tropical dams [J].
Fearnside, Philip M. ;
Pueyo, Salvador .
NATURE CLIMATE CHANGE, 2012, 2 (06) :382-384
[9]   Disrupting biogeochemical cycles -: Consequences of damming [J].
Friedl, G ;
Wüest, A .
AQUATIC SCIENCES, 2002, 64 (01) :55-65
[10]   The impact of dredging deep pits on organic matter decomposition in sediments [J].
Graca, B ;
Burska, D ;
Matuszewska, K .
WATER AIR AND SOIL POLLUTION, 2004, 158 (01) :237-259