Semenkov Ivan, Krupskaya Victoria, Klink Galya
Lomonosov Moscow State University, Russia.
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences, Russia.
Data Brief. 2019 Jul 5;25:104224. doi: 10.1016/j.dib.2019.104224. eCollection 2019 Aug.
Research on migration of chemical elements (ChEs) in soils is important for the understanding of geochemical processes in polluted and undisturbed landscapes. In this article, we report original data on Anthric Chernozems and Anthric Planosols within a small gully's catchment area in the Trans Urals (Russia). Mean total concentrations of 24 ChEs and content of mobile fractions (F1 - exchangeable, F2 - bound within organo-mineral complexes and F3 - bound with Fe and Mn hydroxides) of 61 ChEs including macro elements (Al, Ca, Fe, K, Mg, Mn, Na, P, Ti, S, Si), heavy metals (Ba, Co, Cr, Cu, Ni, Pb, Rb, Sr, Th, U, V, Zn), trace elements (Ag, As, B, Be, Bi, Br, Cd, Cs, Ge, Hf, Li, Mo, Nb, Pd, Sb, Sc, Se, Sn, Ta, Te, Tl, W, Zr) and rare earth elements (Ce, Er, Eu, Gd, La, Lu, Nd, Pr, Sm, Tb, Tm, Dy, Ho, Y, Yb) are determined from in a total of 60 samples from topsoil and subsoil of Anthric Chernozems and Anthric Planosols. The data obtained also include pH-value, total organic carbon content (TOC), seven particle-size classes (<2, 2-6.3, 6.3-20, 20-63, 63-200, 200-630 and 630-2000 μm), electrical conductivity and chemical composition (cations and anions) of water extracts as well as soil mineralogical composition.
研究土壤中化学元素的迁移对于理解污染和未受干扰地区的地球化学过程至关重要。在本文中,我们报告了俄罗斯跨乌拉尔地区一个小流域内人为黑钙土和人为潴育土的原始数据。测定了60个来自人为黑钙土和人为潴育土表土和底土样本中24种化学元素的平均总浓度以及61种化学元素的可移动部分(F1 - 可交换态、F2 - 有机-矿物复合体结合态和F3 - 与铁和锰的氢氧化物结合态)含量,这些化学元素包括大量元素(铝、钙、铁、钾、镁、锰、钠、磷、钛、硫、硅)、重金属(钡、钴、铬、铜、镍、铅、铷、锶、钍、铀、钒、锌)、微量元素(银、砷、硼、铍、铋、溴、镉、铯、锗、铪、锂、钼、铌、钯、锑、钪、硒、锡、钽、碲、铊、钨、锆)和稀土元素(铈、铒、铕、钆、镧、镥、钕、镨、钐、铽、铥钇、镝、钬、钇、镱)。所获得的数据还包括pH值、总有机碳含量(TOC)、七个粒径等级(<2、2 - 至6.3、6.3 - 至20、20 - 至63、63 - 至200、200 - 至630和630 - 至2000μm)、水提取物的电导率和化学成分(阳离子和阴离子)以及土壤矿物组成。