National Geophysical Research Institute (Council of Scientific & Industrial Research), Uppal Road, 500 606, Hyderabad, India.
Environ Monit Assess. 2010 Mar;162(1-4):139-52. doi: 10.1007/s10661-009-0782-3. Epub 2009 Feb 28.
Preliminary investigations were carried out in and around Medak and Sangareddy areas to study the baseline levels of ten major (Si, Al, Ca, Fe, K, Mg, Mn, Na, P, and Ti) and 14 trace elements (As, Ba, Co, Cr, Cu, Mo, Ni, Pb, Rb, Sr, V, Y, Zn, and Zr) on 97 representative soil samples comprising of topsoil (0-25 cm) and subsoil (90-115 cm). The data was factor analyzed for geochemical associations. Because varimax factor loading values show the best results, these were used in interpretation. The derived factors are usually interpreted as associations of elements that imply a common source or behavior in regard to geogenic or anthropogenic influences. It was found that the difference between topsoil and subsoil is not only expressed by concentration differences but also by element associations. Five factors were extracted in topsoil data and account for 80% of the total data variance, while seven factors were extracted in subsoil, which account for 88% of the total variance, suggesting that metal concentration was controlled by soil composition and also that, apart from natural contributions of trace elements to the soils, human activities like agriculture and industrial growth possibly accounted for elemental inputs in soils.
在梅达克和桑加雷迪地区及周边地区进行了初步调查,以研究 97 个具有代表性的土壤样本(包括表土(0-25 厘米)和底土(90-115 厘米))中十种主要元素(Si、Al、Ca、Fe、K、Mg、Mn、Na、P 和 Ti)和 14 种微量元素(As、Ba、Co、Cr、Cu、Mo、Ni、Pb、Rb、Sr、V、Y、Zn 和 Zr)的基线水平。对数据进行了地球化学关联的因子分析。由于方差极大旋转因子负荷值显示出最佳结果,因此这些结果用于解释。所得因子通常被解释为暗示在地球成因或人为影响方面具有共同来源或行为的元素关联。结果发现,表土和底土之间的差异不仅表现在浓度差异上,还表现在元素关联上。在表土数据中提取了五个因子,占总数据方差的 80%,而在底土中提取了七个因子,占总方差的 88%,这表明金属浓度受土壤组成的控制,除了微量元素对土壤的自然贡献外,农业和工业增长等人类活动可能导致土壤中元素的输入。