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Chemical compositions of wet precipitation and anthropogenic influences at a developing urban site in southeastern China

机译:中国东南部发展中城市湿地降水的化学成分和人为影响

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A comprehensive study on the chemical compositions of wet precipitation was carried out from January 2004 to December 2004 in Jinhua, southeastern China's Zhejiang Province. All samples were analyzed for pH, electrical conductivity and major ions (F~-, Cl~-, NO_3~-, SO_4~(2-), K~+, Na~+, Ca~(2+), Mg~(2+) and NH_4~+). The rainwater was typically acidic with a volume-weighted mean pH of 4.54, which ranged from 3.64 to 6.76. SO_4~(2-) and NO_3~- were the main anions, while NH_4~+ and Ca~(2+) were the main cations. The concentrations of these major ions were generally higher compared to those reported in other parts of the world, but much lower than those in northern China. Wet deposition fluxes of major ions showed pronounced seasonal variations with maximum in spring and minimum in autumn. Significant correlations were found in soil-derived species among Ca~(2+), Mg~(2+) and K~+ and sea-salt species between Na~+ and Cl~-. Other relatively good correlations were also observed between Ca~(2+) and SO_4~(2-), Mg~(2+) and SO_4~(2-), Mg~(2+) and NO_3~-, Mg~(2+) and Cl~-. Principal component analysis was also performed on individual precipitation to find possible sources of the major ionic species. Varimax rotated four components accounting for 85.9% of the total variance, and were interpreted as acid and alkaline pollutants, sea spray and mixed source, soil and acideutralization. Calculation of enrichment factors for rainwater components relative to soil and seawater indicated that Ca~(2+) and K~+ mainly originated from the terrestrial source, and SO_4~(2-) and NO_3~- were mostly attributed for the anthropogenic activities in the study area. In general, the results suggested that precipitation chemistry is strongly influenced by anthropogenic sources rather than natural and marine sources. The pollutants in rainwater were mainly derived from long distance transport, local industry and traffic sources.
机译:2004年1月至2004年12月,在中国东南部浙江省金华市对湿降水的化学成分进行了全面研究。分析所有样品的pH,电导率和主要离子(F〜-,Cl〜-,NO_3〜-,SO_4〜(2-),K〜+,Na〜+,Ca〜(2 +),Mg〜( 2+)和NH_4〜+)。雨水通常是酸性的,体积加权平均pH值为4.54,范围为3.64至6.76。 SO_4〜(2-)和NO_3〜-是主要的阴离子,而NH_4〜+和Ca〜(2+)是主要的阳离子。这些主要离子的浓度通常比世界其他地区的浓度高,但比中国北方的浓度低得多。主要离子的湿沉降通量显示出明显的季节变化,春季最大,秋季最小。 Ca〜(2 +),Mg〜(2+)和K〜+之间的土壤来源物种与Na〜+和Cl〜-之间的海盐物种之间存在显着的相关性。 Ca〜(2+)与SO_4〜(2-),Mg〜(2+)与SO_4〜(2-),Mg〜(2+)与NO_3〜-,Mg〜( 2+)和Cl〜-。还对单个降水进行了主成分分析,以找到主要离子物质的可能来源。 Varimax旋转了四个分量,占总方差的85.9%,并被解释为酸和碱污染物,海浪和混合源,土壤和酸/中和。计算雨水相对于土壤和海水的富集因子表明,Ca〜(2+)和K〜+主要来源于陆源,而SO_4〜(2-)和NO_3〜-主要是由于人类活动引起的。学习区。通常,结果表明,降水化学受人为来源而不是天然和海洋来源的强烈影响。雨水中的污染物主要来自长途运输,当地工业和交通来源。

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