中山大学地理科学与规划学院,广州,510275
[ "牛香豫(1997-),女,在读硕士研究生,主要从事流域水循环与水环境研究。E-mail:niuxy8@mail2.sysu.edu.cn" ]
纸质出版:2022
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牛香豫, 唐国平, 顾慧, 等. 流溪河水库流域碳氮营养盐浓度的时空变化特征及其影响因素[J]. 水土保持学报, 2022,36(2):352-360.
NIU Xiangyu, TANG Guoping, GU Hui, et al. Spatial-temporal Variation of Carbon and Nitrogen Nutrients Concentrations and Its Influencing Factors in Liuxi River Reservoir Basin[J]. 2022, 36(2): 352-360.
牛香豫, 唐国平, 顾慧, 等. 流溪河水库流域碳氮营养盐浓度的时空变化特征及其影响因素[J]. 水土保持学报, 2022,36(2):352-360. DOI: 10.13870/j.cnki.stbcxb.2022.02.045.
NIU Xiangyu, TANG Guoping, GU Hui, et al. Spatial-temporal Variation of Carbon and Nitrogen Nutrients Concentrations and Its Influencing Factors in Liuxi River Reservoir Basin[J]. 2022, 36(2): 352-360. DOI: 10.13870/j.cnki.stbcxb.2022.02.045.
流溪河水库流域是亚热带典型的山地河源区
研究此流域的碳氮营养盐浓度时空变化特征及其影响因素对揭示亚热带流域生物地球化学循环与保障水资源供给具有重要意义。基于地形、气象、土地利用、土壤和实地采样获得的水质数据
采用相关分析及Elastic Net回归分析法
探讨了流溪河水库流域溪流碳氮营养盐浓度的时空变化特征及其影响因素。结果表明:(1)从时间上看
枯水期各采样点溪流碳氮营养盐浓度总体变化不大
但空间差异明显
其中NO3-与NH4+浓度具有强相关性。(2)流域坡度大小是引起不同溪流碳氮营养盐浓度存在差异的重要因子
且三级以上坡度对碳氮营养盐浓度变化产生显著的正面影响。(3)流域平均相对湿度也显著影响溪流碳氮营养盐的浓度。流域相对湿度越大
溪流的溶解有机碳浓度相对较高
但氮营养物浓度相对较低;同DOC相比
NO3-和NH4+对气象条件变化敏感度较低。(4)土地利用如建成区面积占比等人类活动显著影响碳氮营养盐的浓度
表现为建成区面积占比与DOC浓度呈负相关关系。此外
森林覆盖度增大会提高溪流DOC和NO3-的浓度
但对NH4+浓度的影响不显著。(5)土壤类型也影响流域碳氮营养盐的浓度
简育低活性强酸土对NO3-浓度产生正面影响
人为堆积土对NH4+浓度产生正面影响。研究结果可为流域水资源保护和了解碳氮营养物浓度的变化及影响因素提供有益信息。
The Liuxi River reservoir basin is a typical subtropical mountain basin
and it is of great significance to study the changing characteristics of carbon and nitrogen nutrients concentrations in this basin and its influencing factors to reveal the biogeochemical cycle of subtropical basin. Based on the field sampling of water quality
landscape topography
meteorology
land use as well as soil data
this paper explored the spatial-temporal changing characteristics and the influencing factors of the carbon and nitrogen nutrients concentrations in streams located in the Liuxi River Reservoir basin
using correlation and Elastic Net regression analysis. The results showed that:(1) The temporal trend of carbon and nitrogen nutrients concentrations in streams was relatively stable during dry period
whereas the spatial variation was obvious. (2) The slope of sub-basin was an important environmental factor that caused the changes of carbon and nitrogen nutrients concentrations in different streams
and the slope beyond 6° had a significant positive effect on the change of carbon and nitrogen nutrients concentrations. (3) The average relative humidity of the basin also significantly affected the concentrations of carbon and nitrogen nutrients in streams. The greater the relative humidity of the basin was
the higher the concentration of carbon nutrients in the streams would be
but the concentration of nitrogen nutrients would be relatively low. Compared witth the DOC
the NH4+ and NO3- concentrations in streams were less sensitive to the weather conditions. (4) The land use
such as the proportion of the built-up area and other human activities
significantly affected the concentrations of carbon and nitrogen nutrients
as shown by a negative correlation between the built-up area and the DOC concentration. The increased forest cover could enhance the DOC and NO3- concentrations in streams
but had no significant effect on the NH4+ concentration. (5) The different soil types also affected the concentrations of carbon and nitrogen nutrients in watersheds
the haplic acrisols had a positive effect on the NO3- concentration
and the aric anthrosols had a positive effect on the concentration of NH4+. Overall
our results provide some useful scientific information for the protection of water resources and understanding the changes and influencing factors of carbon and nitrogen nutrients concentrations in the similar watersheds.
Takagi M, Haga H. Carbon and nitrogen exports from forested headwater catchment in southwestern Japan[J].Biogeochemistry,2019,145(1/2):35-46.
Connolly C T, Khosh M S, Burkart G A, et al. Watershed slope as a predictor of fluvial dissolved organic matter and nitrate concentrations across geographical space and catchment size in the Arctic[J].Environmental Research Letters,2018,13:e104015.
Cheng H, Lin C, Wang L, et al. The influence of different forest characteristics on non-point source pollution:A case study at Chaohu Basin, China[J].International Journal of Environment Research and Public Health,2020,17(5):e1790.
Zarnetske J P, Bouda M, Abbott B W, et al. Generality of hydrologic transport limitation of watershed organic carbon flux across ecoregions of the United States[J].Geophysical Research Letters,2018,45(21):11702-11711.
Dee M M, Tank J L. Inundation time mediates denitrification end products and carbon limitation in constructed floodplains of an agricultural stream[J].Biogeochemistry,2020,149(2):141-158.
dos Santos V M, de Andrade L C, Tiecher T, et al. The urban pressure over the sediment contamination in a Southern Brazil Metropolis:The case of Diluvio stream[J/OL].Water Air and Soil Pollution,2020,231(4):156. DOI:10.1007/s11270-020-04504-2.
Gao T G, Kang S C, Zhang Y L, et al. Characterization, sources and transport of dissolved organic carbon and nitrogen from a glacier in the Central Asia[J].Science of the Total Environment,2020,725:e138346.
Aitkenhead-Peterson J A, Steele M K. Dissolved organic carbon and dissolved organic nitrogen concentrations and exports upstream and downstream of the Dallas-Fort Worth metropolis, Texas, USA[J].Marine and Freshwater Research,2016,67(9):1326-1337.
Rizinjirabake F, Tenenbaum D E, Pilesjo P. Sources of soil dissolved organic carbon in a mixed agricultural and forested watershed in Rwanda[J/OL].Catena,2019,181. DOI:10.1016/j.catena.2019.104085.
Liu K S, Liu Y Q, Jiao N Z, et al. Bacterial community composition and diversity in Kalakuli, an alpine glacial-fed lake in Muztagh Ata of the westernmost Tibetan Plateau[J/OL].Fems Microbiology Ecology,2017,93(7). DOI:10.1093/femsec/fix085.
温展明,徐健荣,林秋奇,等.流溪河水库敞水区轮虫多样性与群落的动态特征[J].生态学报,2017,37(4):1328-1338.
王艳杰,唐红渠,姜仕军.流溪河水库沉积物粒度的时空分布及其沉积动力学意义[J].生态科学,2015,34(3):1-6.
Strohmenger L, Fovet O, Akkal-Corfini N, et al. Multitemporal relationships between the hydroclimate and exports of carbon, nitrogen, and phosphorus in a small agricultural watershed[J].Water Resources Research,2020,56(7):1-17.
卓泉龙,林罗敏,王进,等.广州流溪河氮磷浓度的季节变化和空间分布特征[J].生态学杂志,2018,37(10):3100-3109.
中华人民共和国自然资源部.第三次全国国土调查技术规程TD/T 1055-2019 [S/OL].[2019-01-28 ]. https://www.biao-zhun.cn/637.html.
贾俊平,何晓群,金勇进.统计学[M].4版.北京:中国人民大学出版社,2009.
Zou H, Hastie T. Regularization and variable selection via the elastic net[J].Journal of the Royal Statistical Society Series B-Statistical Methodology,2005,67:301-320.
Lv S C, Wang F, Yan W J, et al. DOC fluorescence properties and degradation in the Changjiang River Network, China:Implications for estimating in-stream DOC removal[J].Biogeochemistry,2019,145(3):255-273.
Osburn C L, Atar J N, Boyd T J, et al. Antecedent precipitation influences the bacterial processing of terrestrial dissolved organic matter in a North Carolina estuary[J].Estuarine Coastal and Shelf Science,2019,221:119-131.
Bol R, Lucke A, Tappe W, et al. Spatio-temporal variations of dissolved organic matter in a German forested mountainous headwater catchment[J].Vadose Zone Journal,2015,14(4):1-12.
Bhattacharya R, Osburn C L. Spatial patterns in dissolved organic matter composition controlled by watershed characteristics in a coastal river network:The Neuse River Basin, USA[J].Water Research,2020,169:e115248.
Muwamba A, Amatya D M, Ssegane H, et al. Response of nutrients and sediment to hydrologic variables in switchgrass intercropped pine forest ecosystems on poorly drained soil[J/OL].Water Air and Soil Pollution,2020,231(9):458. https://doi.org/10.1007/s11270-020-04808-3.
Covino T. Hydrologic connectivity as a framework for understanding biogeochemical flux through watersheds and along fluvial networks[J].Geomorphology,2017,277:133-144.
Sedighi F, Darvishan A K, Zare M R. Effect of watershed geomorphological characteristics on sediment redistribution[J].Geomorphology,2021,375:e107559.
Becerra-Rodas C, Little C, Lara A, et al. The role of streamside native forests on dissolved organic matter in forested and agricultural watersheds in Northwestern Patagonia[J/OL].Forests,2019,10(7):595. DOI:10.3390/f10070595.
Siddiqui E, Pandey J, Pandey U, et al. Integrating atmospheric deposition-driven nutrients (N and P), microbial and biogeochemical processes in the watershed with carbon and nutrient export to the Ganga River[J].Biogeochemistry,2020,147(2):149-178.
Fovet O, Cooper D M, Jones D L, et al. Dynamics of dissolved organic matter in headwaters:Comparison of headwater streams with contrasting DOM and nutrient composition[J/OL].Aquatic Sciences,2020,82(2). DOI:10.1007/s00027-020-0704-6.
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