An evaluation of the hysteresis in chemical concentration-discharge (C-Q) relationships from drained, intensively managed grasslands in southwest England

被引:9
作者
Eludoyin, Adebayo O. [1 ]
Griffith, Bruce [2 ]
Orr, Robert J. [2 ]
Bol, Roland [3 ]
Quine, Timothy A. [4 ]
Brazier, Richard E. [4 ]
机构
[1] Obafemi Awolowo Univ, Dept Geog, Ife, Nigeria
[2] Farm Platform Res Grp, Rothamsted Res, North Wyke, Devon, England
[3] Forschungszentrum, Inst Bio & Geosci Agrosphere IBG 3, Julich, Germany
[4] Univ Exeter, Coll Environm & Life Sci, Dept Geog, Exeter, Devon, England
来源
HYDROLOGICAL SCIENCES JOURNAL-JOURNAL DES SCIENCES HYDROLOGIQUES | 2017年 / 62卷 / 08期
基金
英国生物技术与生命科学研究理事会;
关键词
C-Q relationships; hysteresis; hydrological processes; farm-scale hydrology; SEDIMENT CONCENTRATION; PHOSPHORUS TRANSFERS; SPATIAL VARIABILITY; WATER DISCHARGE; SOIL PROPERTIES; DOUBLE PARADOX; FARM-SCALE; CATCHMENT; RUNOFF; QUALITY;
D O I
10.1080/02626667.2017.1313979
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This study examined the hysteresis exhibited in concentration-discharge (C-Q) relationships in the runoff from four hydrologically separated fields (catchments) at an intensively managed grassland. The objectives were to examine C-Q relationships constructed from high-resolution time series of flow, temperature, pH, conductivity, nitrate and turbidity, and their implications for hydrological processes. High-resolution datasets from the quality assured records of the Rothamsted Research North Wyke Farm Platform in the UK were examined using a graphical method and cross-correlation statistics. The study found that storm events based C-Q hysteresis reflects the cross-correlation that is generally hidden in time series analysis of large datasets, and that although Q and water quality variables can be effectively influenced by catchment size, the C-Q relationship is less significantly influenced. The dominant C-Q relationships of the water variables in the study area reflect that saturated overland flow was prevalent during the study period in the catchments, while the CCF results indicate coupled transfer of sediments and solute in the area at lag 0.<disp-quote>EDITOR D. KoutsoyiannisASSOCIATE EDITOR M. D. Fidelibus</disp-quote
引用
收藏
页码:1243 / 1254
页数:12
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