Cadmium soil sorption at low concentrations: VIII. correlation with soil parameters

Cadmium distribution coefficients, K _d were determined at low Cd concentrations (solute: 0.2 to 3.0 μg Cd dm^?3, soil: 0.044 to 1.1 mg Cd kg^?1) for 63 Danish agricultural soils. The K _d values ranged from 15 to 2450 L kg^?1. About 40% of the soils had K _d values below 200 L kg^?1. The observed K _d values correlated very well with soil pH (r ² = 0.72). Introducing soil organic matter content as a second parameter improved the correlation some (r ² = 0.79). No further improvements were obtained by introducing traditional soil parameters as clay, silt, fine sand, coarse sand and CEC or ‘reactive’ parameters as oxyhydroxides of Mn, Fe and Al. The identified regression equation for predicting K _d values indicates that K _d approximately doubles for each 0.5 unit increase in pH or 2% increase (weight basis) in organic matter content.     

Cadmium soil sorption at low concentrations: VI. A model for zinc competition

Previously presented evidence of Zn competition for Cd soil sorption sites has been confirmed by detailed studies of two Danish soils. Cadmium distribution between soil and solute decreases for increasing Zn solute concentrations. A Langmuir model accounting for both Cd and Zn sorption onto the same sorption sites was supported by independent experimental data on Cd and Zn distribution. The competition of Zn is governed by the product of the Zn soil sorption stability constant and the actual Zn solute concentration. Cadmium distribution coefficients may be significantly influenced by Zn at Zn solute concentrations above 100 μg Zn dm^?3. This may have implications for interpreting Cd plant uptake and leaching.     

Cadmium soil sorption at low concentrations: V. Evidence of competition by other heavy metals

Sorption of Cd at low concentrations onto 12 Danish soils (coarse sands to sandy loams) was studied with respect to competitive effects of other heavy metals by means of laboratory batch experiments. Both a mixture of Ni, Co, and Zn and of Cr, Cu, and Pb effectively reduced the sorption of Cd onto the soils. The employed mixtures of competing heavy metals were considered to resemble moderately polluted conditions. Cadmium distribution coefficients were reduced 2 to 14 times due to competition, but at constant concentrations of competing heavy metals the shape of Cd isotherms was not affected. The effect of Ni, Co, and Zn, which like Cd is primarily governed in soil environments by sorption, was also studied individually. Apparently Zn, which is present in relatively higher concentrations than Ni and Co, accounts for most of the observed competition with Cd.     

Cadmium soil sorption at low concentrations. VII: Effect of stable solid waste leachate complexes

Soil sorption of Cd in solid waste leachates of landfill, sewage sludge, and incinerator residue was studied in the laboratory with emphasis on the behavior of Cd present as stable complexes. A previously developed speciation method was employed to determine free divalent Cd and complexed Cd of various stability. The experiments involved 13 soils covering a wide range of clay contents. Speciation of Cd present in solution after exposure to increasing amounts of soil showed that stable Cd complexes did not sorb onto the soil. This was supported by equilibrium isotherms exhibiting similar solute concentration intercepts and by a leaching study of soil columns which resulted in the same concentration of stable Cd complexes. The stable complexes were of the order of 1 to 10 μg Cd L^?1, the higher values found in landfill and sewage sludge leachate. Very little Cd present in the leachates was free divalent Cd (a few percent), which may explain the low Cd distribution coefficients (3 to 70 L kg^?1).     

Cadmium soil sorption at low concentrations. IV. Effect of waste leachates on distribution coefficients

Field and laboratory studies were conducted to assess the survival of B.t. var. kurstaki in waters. B.t. var. kurstaki was recovered from rivers and public water distribution systems following aerial application of a commercial B.t. formulation (Thuricide 16B). Laboratory studies indicate that B.t. var. kurstaki can survive for relatively long periods of time in fresh water and the marine environment at 20 °C. The amount of residual Cl normally applied to a standard water purification system does not appear to be sufficient to destroy B.t. var. kurstaki. A total Cl residual of at least 1.5 mg L^?1 and 60 min contact time was needed to inactivate 99% of the B. t. var. kurstaki population in tap water at pH 7.2 and 20 °C.     

Cadmium soil sorption at low concentrations: I. Effect of time,cadmium load,pH, and calcium

Sorption of Cd at low concentrations onto two Danish soils (loamy sand, sandy loam) was examined in terms of kinetics and governing factors. From an environmental point of view soil sorption of Cd is a fast process: More than 95% of the sorption takes place within 10 min, equilibrium is reached in 1 hr, and exposures up to 67 wk did not reveal any long term changes in Cd sorption capacities. The soils have very high affinity for Cd at pH = 6.00 (10^?3 M CaCl₂) exhibiting distribution coefficients in the order of 200 to 250 (soil Cd concentration/solute Cd concentration). However, the sorption isotherms describing the distribution of Cd between soil and solute are slightly curvelinear. In the pH-interval 4 to 7.7, the sorption capacity of the soil approximately increases 3 times for a pH increase of one unit. Increasing the Ca concentration from 10^?3 to 10^?2 M reduces the sorption capacity of the sandy loam to one third.     

Cadmium soil sorption at low concentrations: II. Reversibility,effect of changes in solute composition,and effect of soil aging

Water, Air, & Soil Pollution - Desorption of Cd from two Danish soils (loamy sand, sandy loam) previously exposed to low concentrations of Cd was examined in terms of reversibility, effect of...     

The adsorption of copper by soil samples from scotland at low equilibrium solution concentrations

At low solution concentrations of copper in the presence of 0.05 M CaCl₂, adsorption isotherms for copper on soil samples were essentially linear. Although no direct correlations were found between isotherm gradients and individual soil properties, the gradients were of the same order of magnitude as predictions based on gradients obtained for some specific soil components. The soil components which appear to be most important in copper adsorption and which were used to obtain the predictions were organic matter and iron and manganese oxides. The amounts of adsorbed copper remaining isotopically exchangeable or extractable with EDTA in the short term increased with the amount of copper adsorbed but the proportions of adsorbed copper estimated by each of these techniques remained constant. Concentrations of copper in solution increased (adsorption decreased) at pH values below 4.5 and above 6.5.     

Cadmium sorption behavior of natural and synthetic zeolites

Abstract

The sorptive properties of zeolites (a natural zeolite and 3 synthetic zeolites) for cadmium (Cd) were investigated with the intention of selecting suitable materials, for use as amendments in contaminated soils, to reduce the uptake of Cd by field crops. The Cd sorption data were well described by the Langmuir and the Freundlich equations and the coefficients values indicated significant sorptive capacities for Cd by these minerals. Synthetic zeolites have 100 to 500 times greater sorption capacities than the natural zeolite. In all cases, sorption increased with increasing pH and this relationship was linear over the pH range between 3 and 10 for the natural zeolite whereas for the synthetic zeolites a sharp increase was observed between pH 3 and 6. The critical pH above which maximum Cd sorption occurred on synthetic zeolites coincided with the pH where mineral dissolution ceases. The natural zeolite showed an inverse relationship between particle size (<0.15–2.0 mm) and Cd sorption. In desorption experiments with natural zeolite, 10 sequential extractions with 0.01 MNaC10₄ removed 19% Cd from the lowest sorption treatment and 44% of the metal from the highest level, showing that Cd was bound more strongly with decreasing concentrations. Desorption was greater with 0.01 MKC10₄than 0.01 MNaC10₄ especially in the first 5 extractions.     

Phytoremediation of soil contaminated with low concentrations of radionuclides

Primary sludge, secondary sludge, and wood ash from a pulp and paper mill were combined with sand to create a synthetic topsoil (C:N ratio of 18:1) to restore an abandoned gravel pit. Synthetic topsoil was applied to field microcosms at rates equivalent to 0, 2170, 4341, or 6511 kg N/ha; each was seeded with grass. Fifteen chemical constituents in leachate were measured during two field seasons. Cadmium, Ni and Zn were mobilized rapidly by soil disturbance. Chloride and SO₄-S eluted rapidly from the sludge along with Na. Nitrate leached with Ca late in each field season when sludge N-mineralization and nitrification exceeded plant uptake and microbial immobilization. Ammonium elution was negligible. Dissolved organic carbon (DOC) was mobilized by decomposition of organic matter in the sludge, as were Mg and K. Copper eluted with DOC, probably as an organic ligand. Lead and ortho-P were below our detection limits. We concluded that a synthetic topsoil with a 30:1 C:N ratio applied at a rate of 2100-4300 kg N/ha should provide adequate plant nutrition while minimizing water quality hazards.     

Determination of low concentrations of organic phosphorus in soil solution

Abstract

Phosphorus (P) export from agricultural land is an important source of water‐quality deterioration in many areas of the world. Part of the total phosphorus in the soil solution is represented by dissolved organic P at concentrations that can be as low as 1x10^‐6 M of P. The suitability of four digestion methods for the destruction of organic P and determination of orthophosphate at low concentrations and small volumes using the malachite green method has been evaluated. The acid digestion procedures evaluated were 1) sulfuric and perchloric acid, 2) sulfuric acid and potassium persulphate, 3) nitric acid, and 4) nitric and perchloric acid. As inositol hexaphosphate (IHP) represents one of the more resistant molecules to acid hydrolysis in soils, this compound has been chosen to assess the recovery assay of the recommended procedure. The digestion procedures were adapted for the malachite green spectrophotometric method, in order to obtain lower analytical limits for P determination. The sulfuric‐perchloric acid digestion gave excellent recovery and reproducibility, and can therefore be used for determining organic P in solution at concentrations as low as 6.45x10^‐7 M.     

Influence of soil moisture on sorption and degradation of hexazinone and simazine in soil.

Sorption and degradation rates of hexazinone and simazine on soil were determined in a sandy loam soil incubated, during 44 days, at 25 degrees C with moisture contents ranging from 4% to 18%. Herbicide levels in soil solution were also measured, after extraction of this solution by a centrifugation method. All experiments were conducted with treated soil in plastic columns, and the results showed that this method is suitable for the simultaneous study of pesticide sorption and degradation in soil at different environmental conditions. In general, sorption of both herbicides was higher for aged herbicide residues compared to recently applied herbicides, and soil subjected to drying and rewetting cycles had the highest sorption values. K(f) values ranged from 0.5 to 1.2 for simazine and from 0.2 to 0.4 for hexazinone. Degradation rates increased with soil moisture content for both herbicides, and drying-rewetting of soil yielded degradation rates slower than that obtained at 10% soil moisture content. Hexazinone concentration in soil solution decreased with incubation time faster than simazine.     

Chlorine concentrations in alfalfa herbage and soil with KCl topdressing of a low fertility silt loam soil

Abstract

The purpose of this study was to determine the amount of Cl in plants and soil following topdressing of alfalfa with increasing amounts of KCl (0–0–60). The study was conducted with Ranger alfalfa on a low K Piano silt loam soil that had been topdressed twice during three years with a total of zero, 203, 406, 1220, and 2034 kg/ha of Cl as KCl (0, 224, 448, 1334, and 2240 kg/ha of K). Herbage was harvested annually three times at first flower plus an early October cut (4 cuts). The 3‐year average herbage yields were highest with 1220 kg/ha of topdressed Cl. Herbage yields decreased with 2034 kg/ha of Cl, but not significantly below that at 1220 kg/ha. Weakened and yellowed plants were noted in the spring of the second harvest year after 2034 kg/ha of Cl had been applied, and the first‐flower herbage contained 1.90% Cl. It was concluded that the weakened condition of the alfalfa was due to excess Cl.

Movement of Cl through the silt loam soil was rapid. The largest concentrations of Cl in the soil two years after the last KCl application were at the 76 to 91‐cm soil depth, the deepest soil sample tested.     

Addition of phosphorus to soils with low to medium phosphorus retention capacities. I. effect on soil phosphorus sorption properties

Abstract

Twelve soils with low‐medium phosphorus (P) retention capacities were equilibrated for 3 months with soluble phosphate at a rate of 100 mg P kg^‐1 soil. The P sorption properties of these soils both with and without added P were studied, including equilibrium P concentration (EPCo), standard P requirement (SPR), soil P sorption capacity (b), maximum buffer capacity (MBC), and P sorption index (P‐SI). In general, the soils with no added P showed low values of all the above parameters. Oxalate extractable aluminum appeared to be the major responsible element for the control of P sorption in these soils. The addition of P to these soils had a considerable effect on their P sorption properties. The changes in EPCo were well correlated with P sorption index (r=0.80; p≤0.01 ). The EPCo values of the soils with and without added P were closely correlated to bicarbonate extractable P (P_0lsen) and calcium chloride extractable P (P_CaC12), with r=0.80, and r=0.99 (p≤0.001), respectively. Ninety percent of the variability in EPCo was explained by the corresponding variability in P_Olsen when a curvilinear relationship was adopted. The P sorption properties examined appear to be useful parameters to assess the environmental impact of soil P on the quality of surface waters.     

Flupyrsulfuron soil dissipation and mobility in winter wheat crops.

Residues of the sulfonylurea herbicide flupyrsulfuron were extracted from cropping soils with 0.1 M NaHCO(3). The soil extracts were cleaned up by partitioning and repeated thin-layer chromatography. Flupyrsulfuron was transformed by diazomethane into N-(4, 6-dimethoxypyrimidine-2-yl)-N-(3-methoxycarbonyl-6-trifluoromet hylpyr idine-2-yl)methylamine (2), which was analyzed by gas-liquid chromatography with electron capture detection, and confirmation for several samples was made by gas chromatography combined with mass spectrometry. The sensitivity limit was 0.5 microg of flupyrsulfuron kg(-)(1) of dry soil. Bioassays using sugar beet as test plant qualitatively confirmed the results of the chemical analyses. Flupyrsulfuron [10 g of active ingredient ha(-)(1)] was applied in autumn on plots in two winter wheat crops on a sandy loam soil, the first crop being made in 1996-1997 and the second one in 1997-1998. In the 0-8 cm surface soil layer of both crops, the flupyrsulfuron soil half-lives were 123 and 92 days, respectively. Flupyrsulfuron was also applied post-emergence in March to other plots in the same crops; the half-lives in the 0-8 cm surface soil layer were similar in both seasons, that is, approximately 58 days. During all crop trials, flupyrsulfuron remained in the 0-8 cm surface soil layer and was not detected in the 8-10, 10-15, and 15-20 cm surface soil layers. The surface-2 cm soil layer contained the greatest flupyrsulfuron soil concentration, but the residues progressively moved down into the 2-4 and 4-6 cm soil layers. At the winter wheat harvest date for each trial, flupyrsulfuron was not detected in any of the soil layers (<0.5 microg kg(-)(1)).     

Biochar-induced soil phosphate sorption and availability depend on soil properties: a microcosm study

Journal of Soils and Sediments - The effects of soil properties on biochar-induced soil phosphate sorption and availability are not well investigated. An alkaline biochar-induced soil phosphate...     

Speciation and calcium competition effects on cadmium sorption by sandy soil at various pHs

The effects of Ca competition, ionic strength, inorganic complexation and pH on cadmium adsorption by a sandy soil were studied. Sorption of Cd was measured using four different electrolytes CaCl₂, Ca(NO₃)₂, NaNO₃ and NaCl at a constant ionic strength (I) of 0.003 M at three different pHs, at variable Ca/Na ratio with a constant ionic strength of 0.03 and at variable ionic strengths between 0.003 and 0.3 M for two different pHs for Ca(NO₃)₂ and NaNO₃. The measured Cd sorption isotherms were non-linear. In the case of Cl as electrolyte anion, 13% of the Cd in solution is complexed at I= 0.003 (0.002 M Cl) and 91% of Cd is complexed at I= 0.3 (0.2 M Cl). If NO₃ is the anion, none of Cd is complexed at I= 0.003 and 11% at I= 0.3. The Cd complexes do not adsorb significantly. Calcium competition, at an ionic strength of 0.03, reduced the Cd adsorption by 60–80% compared with the case that Na is the cation. Increasing the ionic strength from 0.003 to 0.3 decreased Cd sorption by 60% for Ca(NO₃)₂ and 25% for NaNO₃ due to a decrease of the activity coefficient, increase of inorganic complexation and increase of Ca competition. A decrease of one pH unit reduces Cd sorption of about 75%. Sorption of Cd by soil could be described adequately with the three-species Freundlich (3SF) equation in which pH, complexation, Ca competition and ionic strength effects were taken into account.     

Calculated sulfur dioxide equilibria at low concentrations between air and water

Low concentration equilibria of SO₂ between air and water have been calculated for temperatures in the range 0 to 60°C and air concentrations of 2 ppb to 100 ppm incorporating the best currently available theory to define this process. The data showed negative, non-regular deviations of from less than 1 to about 12% lower than the limited experimental aqueous concentration data available at these levels. Log-log plots of these equilibrium data were linear over a four decade concentration span in air and provided a format which may be readily interpolated for data access. Linear plots of the fraction of the total aqueous SO₂ present as unreacted SO₂ presented here for the first time, show a more marked rise with concentration than was expected, which is used to qualitatively explain biological and corrosion activity of dilute solutions of SO₂.