Distribution and mobility of arsenic in soils of a mining area (Western Spain).

High levels of total and bioavailable As in soils in mining areas may lead to the potential contamination of surface water and groundwater, being toxic to human, plants, and animals. The soils in the studied area (Province of Salamanca, Spain) recorded a total As concentration that varied from 5.5mg/kg to 150mg/kg, and water-soluble As ranged from 0.004mg/kg to 0.107mg/kg, often exceeding the guideline limits for agricultural soil (50mg/kg total As, 0.04mg/kg water-soluble As). The range of As concentration in pond water was <0.001microg/l-60microg/l, with 40% of samples exceeding the maximum permissible level (10microg/l) for drinking water. Estimated bioavailable As in soil varied from 0.045mg/kg to 0.760mg/kg, around six times higher than water-soluble As fraction, which may pose a high potential risk in regard to its entry into food chain. Soil column leaching tests show an As potential mobility constant threatening water contamination by continuous leaching. The vertical distribution of As through soil profiles suggests a deposition mechanism of this element on the top-soils that involves the wind or water transport of mine tailings. A similar vertical distribution of As and organic matter (OM) contents in soil profiles, as well as, significant correlations between As concentrations and OM and N contents, suggests that type and content of soil OM are major factors for determining the content, distribution, and mobilization of As in the soil. Due to the low supergenic mobility of this element in mining environments, the soil pollution degree in the studied area is moderate, in spite of the elevated As contents in mine tailings.

[1]  H. Hapke Heavy metal transfer in the food chain to humans , 1996 .

[2]  A. Garcia-sanchez,et al.  Evaluation of various chemical extraction methods to estimate plant-available arsenic in mine soils. , 2008, Chemosphere.

[3]  S. Tamaki,et al.  Environmental biochemistry of arsenic. , 1992, Reviews of environmental contamination and toxicology.

[4]  E. Smith,et al.  Arsenic in the Soil Environment: A Review , 1998 .

[5]  G. Hall,et al.  Trace elements in water, sediments, porewater, and biota polluted by tailings from an abandoned gold mine in British Columbia, Canada , 1995 .

[6]  E. Álvarez-ayuso,et al.  Sorption of As (V) by some oxyhydroxides and clay minerals. Application to its immobilization in two polluted mining soils , 2002, Clay Minerals.

[7]  D. Mishra,et al.  Effect of dissolved organic matter on the adsorption and stability of As(V) on manganese wad , 2006 .

[8]  Haw-Tarn Lin,et al.  Complexation of arsenate with humic substance in water extract of compost. , 2004, Chemosphere.

[9]  I. Jonasson,et al.  The geochemistry of arsenic and its use as an indicator element in geochemical prospecting , 1973 .

[10]  P. Nye Soil chemistry , 1980, Nature.

[11]  D. Adriano Trace elements in terrestrial environments , 2001 .

[12]  Banfield,et al.  Distribution of thiobacillus ferrooxidans and leptospirillum ferrooxidans: implications for generation of acid mine drainage , 1998, Science.

[13]  Markus Bauer,et al.  Mobilization of arsenic by dissolved organic matter from iron oxides, soils and sediments. , 2006, The Science of the total environment.

[14]  K. Johannesson,et al.  Arsenic Geochemistry of the Great Dismal Swamp, Virginia, USA: Possible Organic Matter Controls , 2007 .

[15]  Donald L. Sparks,et al.  Arsenate and Chromate Retention Mechanisms on Goethite. 2. Kinetic Evaluation Using a Pressure-Jump Relaxation Technique , 1997 .

[16]  H. Tributsch,et al.  Interfacial activity and leaching patterns of Leptospirillum ferrooxidans on pyrite. , 2004, FEMS microbiology ecology.

[17]  R. Oremland,et al.  Bacterial Dissimilatory Reduction of Arsenic(V) to Arsenic(III) in Anoxic Sediments , 1996, Applied and environmental microbiology.

[18]  D. C. Rupainwar,et al.  Adsorption technique for the treatment of As(V)-rich effluents , 1996 .

[19]  L. Deuel,et al.  Arsenic Solubility in a Reduced Environment 1 , 1972 .

[20]  B. E. Davies Applied soil trace elements , 1980 .

[21]  A. Garcia-sanchez,et al.  Arsenic Bioavailability in Polluted Mining Soils and Uptake by Tolerant Plants (El Cabaco mine, Spain) , 2007, Bulletin of environmental contamination and toxicology.

[22]  G. Zagury,et al.  Arsenic speciation and mobilization in CCA-contaminated soils: influence of organic matter content. , 2006, The Science of the total environment.

[23]  S. Goldberg,et al.  Anion sorption on a calcareous, montmorillonitic soil-arsenic , 1988 .

[24]  A. Lowengart,et al.  Fertilizers and Environment , 1996, Developments in Plant and Soil Sciences.

[25]  A. A. Santelises,et al.  Cation exchange capacity. , 1987 .

[26]  J. Hering,et al.  Adsorption of arsenic onto hydrous ferric oxide : effects of adsorbate/adsorbent ratios and co-occurring solutes , 1996 .

[27]  Eugenia Valsami-Jones,et al.  Arsenic pollution sources. , 2008, Reviews of environmental contamination and toxicology.

[28]  Gennaro Brunetti,et al.  Influence of texture on organic matter distribution and quality and nitrogen and sulphur status in semiarid Pampean grassland soils of Argentina , 2004 .

[29]  P. C. Kearney,et al.  CORRELATION BETWEEN AVAILABLE SOIL ARSENIC, ESTIMATED BY SIX METHODS, AND RESPONSE OF CORN (ZEA MAYS L.) , 1971 .

[30]  Klaus Kaiser,et al.  Dissolved organic matter sorption on sub soils and minerals studied by 13C‐NMR and DRIFT spectroscopy , 1997 .

[31]  G. A. Parks,et al.  Solubility and stability of scorodite, FeAsO4.2H2O: Discussion , 1987 .

[32]  S. Goldberg,et al.  Arsenic(iii) and Arsenic(v) Adsorption on Three California Soils , 1997 .

[33]  B. J. Alloway,et al.  Field trials to assess the uptake of arsenic by vegetables from contaminated soils and soil remediation with iron oxides. , 2003, The Science of the total environment.

[34]  K. Tozawa,et al.  On the Solubility Products of Ferric, Calcium and Magnesium Arsenates , 1978 .

[35]  D. Sparks,et al.  Arsenate and Chromate Retention Mechanisms on Goethite. 1. Surface Structure , 1997 .

[36]  C. I. Rich Soil Chemical Analysis , 1958 .

[37]  R. H. Loeppert,et al.  Arsenite and Arsenate Adsorption on Ferrihydrite: Kinetics, Equilibrium, and Adsorption Envelopes , 1998 .

[38]  A. Kabata-Pendias,et al.  Soil-plant transfer of trace elements—an environmental issue , 2004 .

[39]  R. Bowell Sorption of arsenic by iron oxides and oxyhydroxides in soils , 1994 .

[40]  W. Pickering,et al.  Arsenic sorption by humic acids , 1986 .

[41]  R. Delaune,et al.  Effect of redox potential and pH on arsenic speciation and solubility in a contaminated soil , 1991 .

[42]  K. Seshaiah,et al.  Mobility of adsorbed arsenic in two calcareous soils as influenced by water extract of compost. , 2008, Chemosphere.

[43]  J. Ranville,et al.  Evidence for the aquatic binding of arsenate by natural organic matter-suspended Fe(III). , 2006, Environmental science & technology.

[44]  D. B. Harper,et al.  BHC residues of domestic origin: A significant factor in pollution of freshwater in Northern Ireland , 1977 .

[45]  D. V. Naylor,et al.  Sorption and Redox Transformation of Arsenite and Arsenate in Two Flooded Soils , 1994 .

[46]  H. Solo-Gabriele,et al.  Interactions of arsenic and the dissolved substances derived from turf soils. , 2006, Environmental science & technology.

[47]  K. Kalbitz,et al.  Mobilization of heavy metals and arsenic in polluted wetland soils and its dependence on dissolved organic matter. , 1998, The Science of the total environment.

[48]  L. D. Tyler,et al.  MOBILITY AND EXTRACTABILITY OF CADMIUM, COPPER, NICKEL, AND ZINC IN ORGANIC AND MINERAL SOIL COLUMNS , 1982 .

[49]  A. Garcia-sanchez,et al.  Arsenic in soils and waters and its relation to geology and mining activities (Salamanca Province, Spain) , 2003 .

[50]  A. Saada,et al.  Adsorption of arsenic (V) on kaolinite and on kaolinite-humic acid complexes. Role of humic acid nitrogen groups. , 2003, Chemosphere.

[51]  H. Tributsch,et al.  Reasons why 'Leptospirillum'-like species rather than Thiobacillus ferrooxidans are the dominant iron-oxidizing bacteria in many commercial processes for the biooxidation of pyrite and related ores. , 1999, Microbiology.

[52]  L. Ma,et al.  Effects of compost and phosphate on plant arsenic accumulation from soils near pressure-treated wood. , 2004, Environmental pollution.

[53]  G. Gee,et al.  Particle-size Analysis , 2018, SSSA Book Series.

[54]  Shuhua Yao,et al.  Mechanism of arsenate mobilization from goethite by aliphatic carboxylic acid. , 2009, Journal of hazardous materials.

[55]  A. Meharg,et al.  Phosphorus nutrition of arsenate-tolerant and nontolerant phenotypes of velvetgrass , 1994 .

[56]  P. Dove,et al.  The solubility and stability of scorodite, FeAsO 4 .2H 2 O , 1985 .

[57]  A. Garcia-sanchez,et al.  Exposure and bioavailability of arsenic in contaminated soils from the La Parrilla mine, Spain , 2006 .

[58]  M. Berg,et al.  Arsenite and arsenate binding to dissolved humic acids: influence of pH, type of humic acid, and aluminum. , 2006, Environmental science & technology.

[59]  C. Mulligan,et al.  Effect of natural organic matter on arsenic release from soils and sediments into groundwater , 2006, Environmental geochemistry and health.