Arsenic distribution in soils and plants of an arsenic impacted former mining area.

A mining area affected by the abandoned exploitation of an arsenical tungsten deposit was studied in order to assess its arsenic pollution level and the feasibility of native plants for being used in phytoremediation approaches. Soil and plant samples were collected at different distances from the polluting sources and analysed for their As content and distribution. Critical soil total concentrations of As were found, with values in the range 70-5330 mg kg(-1) in the uppermost layer. The plant community develops As tolerance by exclusion strategies. Of the plant species growing in the most polluted site, the shrubs Salix atrocinerea Brot. and Genista scorpius (L.) DC. exhibit the lowest bioaccumulation factor (BF) values for their aerial parts, suggesting their suitability to be used with revegetation purposes. The species Scirpus holoschoenus L. highlights for its important potential to stabilise As at root level, accumulating As contents up to 3164 mg kg(-1).

Arsenic, antimony, and other trace element contamination in a mine tailings affected area and uptake by tolerant plant species.

The study was conducted to characterize mineralogical and elemental composition of mine tailings in order to evaluate the environmental hazards, and identify the metal accumulation potential of native plant species from São Domingos mine, one of the long-term activity mines of the Iberian Pyrite Belt dating back to pre-Roman times. The mine tailings including soils and different plant species from São Domingos were analyzed for determination of tailings characteristics and chemical element contents in tailings and plants. The large amounts of mining wastes are causing significant adverse environment impacts due to acid mine drainage production and mobilization of potentially toxic metals and metalloids in residential areas, agricultural fields, downstreams, and rivers. The typical mineralogical composition is as follows: quartz, micas, K-feldspar, olivine-group minerals, magnetite, goethite, hematite, jarosite, and sulfides. The mine tailings were highly contaminated by As, Ag, Cr, Hg, Sn, Sb, Fe, and Zn; and among them, As and Sb, main contaminants, attained the highest concentrations except Fe. Arsenic has exhibited very good correlations with Au, Fe, Sb, Se, and W; and Sb with As, Au, Fe, Se, Sn, and W in tailings. Among the all plant species, the higher concentrations of all the metals were noted in Erica andevalensis, Erica australis, Echium plantagium, and Lavandula luisierra. Considering the tolerant behavior and abundant growth, the plant species Erica australis, Erica andevalensis, Lavandula luisierra, Daphne gnidium, Rumex induratus, Ulex eriocladus, Juncus, and Genista hirsutus are of major importance for the rehabilitation and recovery of degraded São Domingos mining area.

Evaluation of various chemical extraction methods to estimate plant-available arsenic in mine soils.

Elevated levels of bioavailable As in mining soils, agricultural areas and human habitats may cause potential toxicity to human health, plants and microbe. Therefore, it is essential to determine proper soil chemical extraction method in order to estimate plant-available As in mining soils and protect agricultural and environmental ecosystems by evaluation of environmental risk and implementation of remediation measures. In this study, six single soil chemical extraction processes and four-step sequential chemical extraction protocol were used to determine the relative distribution of As in different chemical forms of soils and their correlations with total As in plants grown in mining areas and greenhouse experiments. The strongest relationship between As determined by single soil chemical extraction and As in plant biomass was found for sodium acetate and mixed acid extractant. The mean percent of total As extracted was: ammonium oxalate (41%)>hydroxylamine hydrochloride (32%)>mixed acid (16%)>phosphate (6%)>sodium acetate (1.2%)>water (0.13%). This trend suggests that most of the As in these soils is inside the soil mineral matrix and can only be released when iron oxides and other minerals are dissolved by the stronger chemical extractant. Single soil chemical extraction methods using sodium acetate and mixed acids, that extract As fractions complexed to soil particles or on the surface of mineral matrix of hydrous oxides of Fe, Mn and Al (exchangeable+sorbed forms) can be employed to estimate and predict the bioavailable As fraction for plant uptake in mining affected soils. In sequential chemical extraction methods, ammonium nitrate and hydroxylamine hydrochloride may be used to provide closer estimates of plant-available As in mining soils.

Leaf water potential and stomatal conductance in Quercus pyrenaica Willd. forests: vertical gradients and response to environmental factors.

Two permanent sampling sites were selected at the two extremes of a rainfall gradient in natural forests of Quercus pyrenaica Willd. located in the Sierra de Gata (Salamanca Province, Spain). During 1991 and 1992, diurnal courses of transpiration rate (E), stomatal conductance (g(s)) and leaf water potential (Psi(l)) were studied at different levels in the tree canopy. Leaf water potential fell from a high value in the early morning to a minimum at midday and then increased again in the afternoon. Values of Psi(l) in the early morning and at midday were lower at Fuenteguinaldo (dry site) than at Navasfrías (wet site) and were related to soil water availability. Stomatal conductance increased during the morning and maximum g(s) occurred about 3 h before Psi(l) was at its lowest value. The highest values of g(s) were found at Navasfrías during July. The lowest Psi(l) values were found in the upper parts of the canopy and differences among canopy levels were greatest when soil water availability was low. In August, minimum values of Psi(l) differed among canopy levels by 1.0 MPa at Navasfrías and by 0.8 MPa at Fuenteguinaldo. The maximum difference in g(s) among canopy levels was about 150 mmol m(-2) s(-1) at Navasfrías and about 300 mmol m(-2) s(-1) at Fuenteguinaldo. The results indicate a nonconservative pattern of water use in Quercus pyrenaica.