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Effects of catchment and riparian landscape setting on water chemistry and seasonal evolution of water quality in the upper Han river basin, China

机译:汉江上游流域和河岸景观环境对水化学和水质季节性变化的影响

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摘要

Six-year (2005–2010) evolution of water chemistry (Cl−, NO3−, SO42−, HCO3−, Na+, K+, Ca2+and Mg2+) and their interactions with morphological properties (i.e., slope and area), land cover, and hydrological seasonality were examined to identify controlling factors and processes governing patterns of stream water quality in the upper Han River, China. Correlation analysis and stepwise multiple regression models revealed significant correlations between ions (i.e., Cl−, SO42−, Na+ and K+) and land cover (i.e., vegetation and bare land) over the entire catchment in both high- and low-flow periods, and in the buffer zone the correlation was much more stronger in the low-flow period. Catchment with steeper slope (\u3e15°) was negatively correlated with major ions, largely due to multicollinearity of basin characteristics. Land cover within the buffer zone explained slightly less of major elements than at catchment scale in the rainy season, whereas in the dry season, land cover along the river networks in particular this within 100 m riparian zone much better explained major elements rather than this over the entire catchment. Anthropogenic land uses (i.e., urban and agriculture) however could not explain water chemical variables, albeit EC, TDS, anthropogenic markers (Cl−, NO3−, SO42), Na+, K+ and Ca2+ significantly increased during 2005–2010, which was corroborated by principal component analyses (PCA) that indicated anthropogenic inputs. Observations demonstrated much higher solute concentrations in the industrial-polluted river. Our results suggested that seasonal evolution of water quality in combined with spatial analysis at multiple scales should be a vital part of identifying the controls on spatio-temporal patterns of water quality.
机译:水化学(Cl-,NO3-,SO42-,HCO3-,Na +,K +,Ca2 +和Mg2 +)的六年(2005-2010年)演变及其与形态学特征(即坡度和面积),土地覆盖的相互作用考察了水文季节,确定了汉江上游河流水质模式的控制因素和控制过程。相关分析和逐步多元回归模型显示,在高流量和低流量期间,整个集水区的离子(即Cl-,SO42-,Na +和K +)与土地覆盖率(即植被和裸地)之间都具有显着的相关性,在缓冲区,低流量时期的相关性要强得多。斜率较大的集水区(\ u3e15°)与主要离子呈负相关,这主要是由于盆地特征的多重共线性所致。在雨季,缓冲区内的土地覆盖解释的主要要素比集水规模要少一些,而在干旱季节,沿河网的土地覆盖尤其是沿河岸带100 m之内的解释要好得多,而不是超过整个集水区。然而,人为的土地利用(即城市和农业)无法解释水的化学变量,尽管EC,TDS,人为标记(Cl-,NO3-,SO42),Na +,K +和Ca2 +在2005-2010年期间显着增加,这得到了证实。通过主成分分析(PCA)表示人为输入。观测结果表明,工业污染河中的溶质浓度更高。我们的研究结果表明,水质的季节性演变与多尺度空间分析相结合,应该是确定水质时空格局控制的重要组成部分。

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