Mercury pollution is widespread globally, and strategies for managing mercury contamination in aq... more Mercury pollution is widespread globally, and strategies for managing mercury contamination in aquatic environments are necessary. We tested whether coagulation with metal-based salts could remove mercury from wetland surface waters and decrease mercury bioaccumulation in fish. In a complete randomized block design, we constructed nine experimental wetlands in California's Sacramento-San Joaquin Delta, stocked them with mosquitofish (Gambusia affinis), and then continuously applied agricultural drainage water that was either untreated (control), or treated with polyaluminum chloride or ferric sulfate coagulants. Total mercury and methylmercury concentrations in surface waters were decreased by 62% and 63% in polyaluminum chloride treated wetlands and 50% and 76% in ferric sulfate treated wetlands compared to control wetlands. Specifically, following coagulation, mercury was transferred from the filtered fraction of water into the particulate fraction of water which then settled within the wetland. Mosquitofish mercury concentrations were decreased by 35% in ferric sulfate treated wetlands compared to control wetlands. There was no reduction in mosquitofish mercury concentrations within the polyaluminum chloride treated wetlands, which may have been caused by production of bioavailable methylmercury within those wetlands. Coagulation may be an effective management strategy for reducing mercury contamination within wetlands, but further studies should explore potential effects on wetland ecosystems.
ABSTRACT The importance of diverse microbial groups to soil C maintenance is still a matter of de... more ABSTRACT The importance of diverse microbial groups to soil C maintenance is still a matter of debate. This study follows the turnover of 13C labeled nonliving residues from diverse microbial groups into soil physical fractions in situ in a temperate forest in California (CA) and a tropical forest in Puerto Rico (PR), during 5 sampling points per site- over a 3 and 2 year period, respectively. Microbial groups include fungi, actinomycetes, Gm(+) bacteria, and Gm(-) bacteria, isolated from CA and PR soils to obtain temperate and tropical isolates composited of 3-4 species per group. The selected density fractionation approach isolated: a "light fraction" (LF), non-mineral aggregate "occluded fraction" (OF), and a "mineral bound fraction" (MF). Pyrolysis gas chromatography mass spectrometry (Py-GC-MS) was employed to characterize microbial group isolates, whole soils, and fractions. Microbial isolates contained unique biochemical fingerprints: temperate and tropical fungi and tropical Gm(-) were characterized by a low abundance of phenol, benzene, and N-compounds compared with other microbial group isolates. Py-GC-MS revealed compositional differences among soil fractions at both sites, likely attributed to differences in the decomposition stage and C source material (ie. plant vs. microbial). For both sites, benzene and N-compounds were greatest in the MF; lignin and phenol compounds were greatest in the LF; and lipids were greatest in the OF. The trend for polysaccharides differed between sites, with the greatest concentration in the CA OF; and for PR with the lowest concentration in the OF, and similar concentrations in the LF and MF. SOM chemistry was most similar between sites in the LF, compared with the OF and MF, suggesting that differences in SOM chemistry between sites may be more attributed to differential decomposition processes than unique litter quality inputs. A substantial portion of microbial C moved from the LF into the OF, and the MF by the first sampling point for both sites. Microbial C inputs were more stable in the OF and MF than the LF throughout the course of the study at both sites. There were no differences in 13C recovery among microbial isolates in any fractions in PR, despite minor differences in overall turnover rates. In CA, there were some differences among microbial isolates in 13C recovery in the LF and OF, which related to 13C recoveries in whole soils. In the CA MF, microbial 13C recoveries did not significantly differ, and in generally low variability among treatments was observed. Results support increased protection of microbial C via association with the MF; however, differential sorption of various microbial group isolates over others was not observed. Overall results suggest that inherent properties of microbial residues may be more important to determining its stability in CA soils when it is 1) unassociated with the mineral matrix (LF); or 2) physically occluded within aggregates; compared with that intimately associated with mineral surfaces (MF). Compound-specific recovery of microbial isolates with Py-GC-MS-IRMS will be discussed.
thereby affecting N sequestration rates into SOM frac- tions and its subsequent turnover. Crop re... more thereby affecting N sequestration rates into SOM frac- tions and its subsequent turnover. Crop residue management practices can affect N immobilization Previous work from long-term rice management stud- and stabilization processes important to efficient utilization of N from
Opencast mining causes severe impacts on natural environments, often resulting in permanent damag... more Opencast mining causes severe impacts on natural environments, often resulting in permanent damage to soils and vegetation. In the present study we use a 14-year restoration chronosequence to investigate how resource input and spontaneous plant colonization promote the revegetation and reconstruction of mined soils in central Brazil. Using a multi-proxy approach, combining vegetation surveys with the analysis of plant and soil isotopic abundances (delta13C and delta15N) and chemical and physical fractionation of organic matter in soil profiles, we show that: (1) after several decades without vegetation cover, the input of nutrient-rich biosolids into exposed regoliths prompted the establishment of a diverse plant community (> 30 species); (2) the synergistic effect of resource input and plant colonization yielded unprecedented increases in soil carbon, accumulating as chemically stable compounds in occluded physical fractions and reaching much higher levels than observed in undisturbed ecosystems; and (3) invasive grasses progressively excluded native species, limiting nutrient availability, but contributing more than 65% of the total accumulated soil organic carbon. These results show that soil-plant feedbacks regulate the amount of available resources, determining successional trajectories and alternative stable equilibria in degraded areas undergoing restoration. External inputs promote plant colonization, soil formation, and carbon sequestration, at the cost of excluding native species. The introduction of native woody species would suppress invasive grasses and increase nutrient availability, bringing the system closer to its original state. However, it is difficult to predict whether soil carbon levels could be maintained without the exotic grass cover. We discuss theoretical and practical implications of these findings, describing how the combination of resource manipulation and management of invasive species could be used to optimize restoration strategies, counteracting soil degradation while maintaining species diversity.
Agriculture, ecosystems & environment, May 31, 1999
The importance of nitrogen (N), weeds, and water as yield-limiting factors was evaluated over a 4... more The importance of nitrogen (N), weeds, and water as yield-limiting factors was evaluated over a 4-year period in tomato cropping systems under conventional, low-input, and organic management. The cropping systems studied were part of the Sustainable Agriculture Farming Systems (SAFS) Project at the University of California, Davis, a comparison of conventional and alternative farming systems in California's Sacramento Valley. Water applied, soil N levels, plant N uptake, weed abundance, and tomato yield were measured ...
Soil chemical properties during the transition from conventional to organic and low-input farming... more Soil chemical properties during the transition from conventional to organic and low-input farming practices were studied over 8 yr in California's Sacramento Valley to document changes in soil fertility status and nutrient storage. Four fanning systems differing in crop rotation and external inputs were established on land previously managed conventionally. Fertility in the organic system depended on animal manure applications and winter cover crops; the two conventional systems received synthetic fertilizer inputs; the low-input ...
Mercury pollution is widespread globally, and strategies for managing mercury contamination in aq... more Mercury pollution is widespread globally, and strategies for managing mercury contamination in aquatic environments are necessary. We tested whether coagulation with metal-based salts could remove mercury from wetland surface waters and decrease mercury bioaccumulation in fish. In a complete randomized block design, we constructed nine experimental wetlands in California's Sacramento-San Joaquin Delta, stocked them with mosquitofish (Gambusia affinis), and then continuously applied agricultural drainage water that was either untreated (control), or treated with polyaluminum chloride or ferric sulfate coagulants. Total mercury and methylmercury concentrations in surface waters were decreased by 62% and 63% in polyaluminum chloride treated wetlands and 50% and 76% in ferric sulfate treated wetlands compared to control wetlands. Specifically, following coagulation, mercury was transferred from the filtered fraction of water into the particulate fraction of water which then settled within the wetland. Mosquitofish mercury concentrations were decreased by 35% in ferric sulfate treated wetlands compared to control wetlands. There was no reduction in mosquitofish mercury concentrations within the polyaluminum chloride treated wetlands, which may have been caused by production of bioavailable methylmercury within those wetlands. Coagulation may be an effective management strategy for reducing mercury contamination within wetlands, but further studies should explore potential effects on wetland ecosystems.
ABSTRACT The importance of diverse microbial groups to soil C maintenance is still a matter of de... more ABSTRACT The importance of diverse microbial groups to soil C maintenance is still a matter of debate. This study follows the turnover of 13C labeled nonliving residues from diverse microbial groups into soil physical fractions in situ in a temperate forest in California (CA) and a tropical forest in Puerto Rico (PR), during 5 sampling points per site- over a 3 and 2 year period, respectively. Microbial groups include fungi, actinomycetes, Gm(+) bacteria, and Gm(-) bacteria, isolated from CA and PR soils to obtain temperate and tropical isolates composited of 3-4 species per group. The selected density fractionation approach isolated: a "light fraction" (LF), non-mineral aggregate "occluded fraction" (OF), and a "mineral bound fraction" (MF). Pyrolysis gas chromatography mass spectrometry (Py-GC-MS) was employed to characterize microbial group isolates, whole soils, and fractions. Microbial isolates contained unique biochemical fingerprints: temperate and tropical fungi and tropical Gm(-) were characterized by a low abundance of phenol, benzene, and N-compounds compared with other microbial group isolates. Py-GC-MS revealed compositional differences among soil fractions at both sites, likely attributed to differences in the decomposition stage and C source material (ie. plant vs. microbial). For both sites, benzene and N-compounds were greatest in the MF; lignin and phenol compounds were greatest in the LF; and lipids were greatest in the OF. The trend for polysaccharides differed between sites, with the greatest concentration in the CA OF; and for PR with the lowest concentration in the OF, and similar concentrations in the LF and MF. SOM chemistry was most similar between sites in the LF, compared with the OF and MF, suggesting that differences in SOM chemistry between sites may be more attributed to differential decomposition processes than unique litter quality inputs. A substantial portion of microbial C moved from the LF into the OF, and the MF by the first sampling point for both sites. Microbial C inputs were more stable in the OF and MF than the LF throughout the course of the study at both sites. There were no differences in 13C recovery among microbial isolates in any fractions in PR, despite minor differences in overall turnover rates. In CA, there were some differences among microbial isolates in 13C recovery in the LF and OF, which related to 13C recoveries in whole soils. In the CA MF, microbial 13C recoveries did not significantly differ, and in generally low variability among treatments was observed. Results support increased protection of microbial C via association with the MF; however, differential sorption of various microbial group isolates over others was not observed. Overall results suggest that inherent properties of microbial residues may be more important to determining its stability in CA soils when it is 1) unassociated with the mineral matrix (LF); or 2) physically occluded within aggregates; compared with that intimately associated with mineral surfaces (MF). Compound-specific recovery of microbial isolates with Py-GC-MS-IRMS will be discussed.
thereby affecting N sequestration rates into SOM frac- tions and its subsequent turnover. Crop re... more thereby affecting N sequestration rates into SOM frac- tions and its subsequent turnover. Crop residue management practices can affect N immobilization Previous work from long-term rice management stud- and stabilization processes important to efficient utilization of N from
Opencast mining causes severe impacts on natural environments, often resulting in permanent damag... more Opencast mining causes severe impacts on natural environments, often resulting in permanent damage to soils and vegetation. In the present study we use a 14-year restoration chronosequence to investigate how resource input and spontaneous plant colonization promote the revegetation and reconstruction of mined soils in central Brazil. Using a multi-proxy approach, combining vegetation surveys with the analysis of plant and soil isotopic abundances (delta13C and delta15N) and chemical and physical fractionation of organic matter in soil profiles, we show that: (1) after several decades without vegetation cover, the input of nutrient-rich biosolids into exposed regoliths prompted the establishment of a diverse plant community (> 30 species); (2) the synergistic effect of resource input and plant colonization yielded unprecedented increases in soil carbon, accumulating as chemically stable compounds in occluded physical fractions and reaching much higher levels than observed in undisturbed ecosystems; and (3) invasive grasses progressively excluded native species, limiting nutrient availability, but contributing more than 65% of the total accumulated soil organic carbon. These results show that soil-plant feedbacks regulate the amount of available resources, determining successional trajectories and alternative stable equilibria in degraded areas undergoing restoration. External inputs promote plant colonization, soil formation, and carbon sequestration, at the cost of excluding native species. The introduction of native woody species would suppress invasive grasses and increase nutrient availability, bringing the system closer to its original state. However, it is difficult to predict whether soil carbon levels could be maintained without the exotic grass cover. We discuss theoretical and practical implications of these findings, describing how the combination of resource manipulation and management of invasive species could be used to optimize restoration strategies, counteracting soil degradation while maintaining species diversity.
Agriculture, ecosystems & environment, May 31, 1999
The importance of nitrogen (N), weeds, and water as yield-limiting factors was evaluated over a 4... more The importance of nitrogen (N), weeds, and water as yield-limiting factors was evaluated over a 4-year period in tomato cropping systems under conventional, low-input, and organic management. The cropping systems studied were part of the Sustainable Agriculture Farming Systems (SAFS) Project at the University of California, Davis, a comparison of conventional and alternative farming systems in California's Sacramento Valley. Water applied, soil N levels, plant N uptake, weed abundance, and tomato yield were measured ...
Soil chemical properties during the transition from conventional to organic and low-input farming... more Soil chemical properties during the transition from conventional to organic and low-input farming practices were studied over 8 yr in California's Sacramento Valley to document changes in soil fertility status and nutrient storage. Four fanning systems differing in crop rotation and external inputs were established on land previously managed conventionally. Fertility in the organic system depended on animal manure applications and winter cover crops; the two conventional systems received synthetic fertilizer inputs; the low-input ...
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