Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Horizontal and Vertical Distributions of Chromium in a Chromate Production District of South Central China

Bibliographic Data

ID15465642
AuthorsBin Zhou (0000-0002-5816-445X, Key Laboratory for Agro-Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China), Zhou Bin (0000-0002-2909-8764, Yonker Environmental Protection (China)), Daoyou Huang (Chinese Academy of Sciences, corresponding author), Jinshui Wu (Chinese Academy of Sciences), Qihong Zhu (0000-0002-6326-8093, Chinese Academy of Sciences), Hanhua Zhu (Chinese Academy of Sciences)
Year2018
Volume15
Issue4
Pages571-571
Publication date2018-03-22
Open AccessYes
TypeARTICLE
VenueInternational Journal of Environmental Research and Public Health (JOURNAL)
Journal identifiersISSN: 1661-7827 • E-ISSN: 1660-4601
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph15040571
PMID29565800
OpenAlexW2790800296
LanguageEN
References cited24

To study the horizontal and vertical distribution of chromium (Cr) in the soil of a chromate production site (CPS) and its nearby area (NA-CPS) in south central China, 61 profiles (depth: 14 m) in the CPS and 69 samples (topsoil) were excavated following a grid-sampling method. The geographic coordinates, elevation, and types of soil layers were recorded, and the total Cr in the soil and the total Cr and Cr(VI) in the leachate of the soil and in the groundwater were determined. Migration of Cr in surface soils may be represented in terms of a multiple linear regression equation ( R 2 adj = 0.632). Distance, elevation, and pH are the primary factors that influence the horizontal distribution of Cr content in the surface soils, while the Cr concentration in different soil profiles mostly obeys the positive or negative binomial distributions. For a positive distribution, the Cr concentration decreases with increasing depth in the 0.0-8.0 m soil layer, under the fixing effect of soil. However, it shows an upward trend with a depth in the 8-14 m soil layer under the influence of Cr-polluted phreatic water. Under a negative distribution, Cr content is stable in the 0-6 m layer because of the influence of chromite ore processing residue mixed with miscellaneous fills, but it decreases obviously in the 6-14 m layer under the fixing effect of soil. Similar vertical distributions were observed for pH, L Cr , L Cr 6+ , and P Cr 6+ . The decreasing amplitude of the Cr concentration for binomial distributions is mainly affected by the Cr concentration, pH, and LR Cr of the soil. Moreover, P Cr 6+ of soil increases with pH, and the type of soil layer is the primary factor influencing LR Cr in the soil profiles. Our results of the horizontal and vertical distributions of Cr could be used to guide investigations that are focused on reducing the number of samples in the horizontal and vertical directions at CPSs, and to improve risk assessments of CPSs and nearby areas

Chromate conversion coating · Chromium · Groundwater · Hydrology (agriculture · Soil horizon · Soil water · Subsoil · Topsoil · Adsorption and biosorption for pollutant removal · Chemistry · Chromium effects and bioremediation · Environmental Science · Heavy metals in environment · Geology · Soil Science

Highly citedNo

Tools

Open DOISci-HubOpen Access
Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae