Phospholipid fatty acid (PLFA) patterns were used to describe the composition of the soil microbial communities under 12 natural forest stands including oak and beech, spruce-fir-beech, floodplain and pine forests. In addition to the quantification of total PLFAs, soil microbial biomass was measured by substrate-induced respiration and chloroform fumigation-extraction. The forest stands possess natural vegetation, representing an expression of the natural site factors, and we hypothesised that each forest type would support a specific soil microbial community. Principal component analysis (PCA) of PLFA patterns revealed that the microbial communities were compositionally distinct in the floodplain and pine forests, comprising azonal forest types, and were more similar in the oak, beech and spruce-fir-beech forests, which represent the zonal vegetation types of the region. In the nutrient-rich floodplain forests, the fatty acids 16:1ω5, 17:0cy, a15:0 and a17:0 were the most prevalent and soil pH seemed to be responsible for the discrimination of the soil microbial communities against those of the zonal forest types. The pine forest soils were set apart from the other forest soils by a higher abundance of PLFA 18:2ω6,9, which is typical of fungi and may also indicate ectomycorrhizal fungi associated with pine trees, and high amounts of PLFA 10Me18:0, which is common in actinomycetes. These findings suggest that the occurrence of azonal forest types at sites with specific soil conditions is accompanied by the development of specific soil microbial communities. The study provides information on the microbial communities in undisturbed forest soils which may facilitate interpretation of data derived from managed or even damaged or degraded forests. 相似文献
Oil hydrocarbons are widespread pollutants in soil which pose serious threats to ecological environment. Thus, this study carried out the bioremediation of oil-contaminated soil by using the efficient petroleum-degrading bacteria and soil conditioner, to investigate the changes of physicochemical properties of contaminated soil during bioremediation, reveal the relationship among the exogenous degradation strains and indigenous microbe, and finally illuminate the effects of soil conditioner and microbe on the bioremediation of oil-contaminated soil.
Materials and methods
A PAH-degrading strain named Stenotrophomonas maltophilia was used in this study, which was isolated from an e-waste dismantling area. The soil conditioner in this present study was developed previously by using agricultural wastes, which was in a powdered form and rich in N, P, and K. The simulated experiments were conducted under the control environmental conditions of greenhouse, to study the effects of inoculation and soil conditioner on bioremediation of oil-contaminated soil. Then, the physicochemical properties of soil and the degradation rates of oil were measured at different set times to evaluate the bioremediation effect.
Results and discussion
Adding 1% soil conditioner could significantly improve the soil conditions and offer microorganism enough N, P, and K, which would promote microbial growth and played a key role on bioremediation of oil-contaminated soil. Although in polluted soil, the microorganism could maintain metabolic activity and use the petroleum as carbon source. The soil indigenous microbe was more easily to adapt to the contaminated surrounding. However, when both of them co-existed in soil, they would restrain each other, and go against the oil decomposition. Thus, making two types of microorganisms work to achieve synergy was the key to gain much better remediation effect. Because the indigenous microbe was good at decomposing low molecular compounds and saturated hydrocarbons, while the oil-degrading strains can effectively decompose high molecular weight aromatics.
Conclusions
The soil nutrient and microorganism, including the exogenous oil-degrading strains and the soil indigenous microbe, had an important effect on degradation of petroleum. The addition of soil conditioner, presence of indigenous microbe, and inoculation of oil-degrading strains all were conducive to bioremediation of oil-contaminated site, but the key was to control the proportion and relationship of the three.
The nature of the main selenium (Se) carrier phases in soil is in debate, with some authors emphasizing the role of minerals, and others the role of organic material. In this study, we address the role of the different soil components in Se sorption by determining its interaction with easily separable and workable fractions of bulk soil. Thus four separated fractions (two organic and two mineral) isolated by size density fractionation from a grassland soil were taken as models for soil Se carrier phases. Two concentrations of selenite were used to estimate its reactivity during experiments. In addition, SEM-TEM analyses (coupled with EDS) were used to determine the chemical environment of Se sorbed onto the different fractions. The results showed that for the smaller selenite concentration nearly all the fractions gave the same selenite sorption (approximately 99%). For the larger concentration, selenite sorption ranged between 44% (mineral fractions) and 93% (organic fractions), indicating that the sorption capacities of organic fractions were greater than those of mineral fractions. In all soil fractions, elementary analyses and SEM/EDS and TEM/EDS observations revealed that Se sorption and the detection of Se hot spots on the soil particles correlated with the presence of Fe and Al. Although a direct association between Se and organic material could not be excluded, we suggest that Se sorption on organic particles is indirect, mainly resulting from association with surface Fe oxides or clays. These findings question the current view of a direct correlation between organic carbon and Se in natural soil samples. 相似文献
Depleted soil fertility and high-yielding cultivars have been associated with low mineral nutrient contents in vegetables. This study explored if mineral nutrient concentrations of lettuce (Lactuca sativa L.) can be increased though selection of cultivars and management of soil fertility. Cultivars including butterhead, romaine, and loose-leaf phenotypes of heritage and modern origins were studied. Conventional, compost, and organic regimes were assessed. Elements in whole heads were determined. Heritage cultivars had about 7% higher magnesium, sulfur, copper, and iron (Mg, S, Cu, and Fe) concentrations than modern cultivars with no differences occurring for phosphorus, potassium, calcium, sodium, zinc, manganese and boron (P, K, Ca, Na, Zn, Mn, and B). Differences for each element occurred among phenotypes and fertilization but with no consistent trends. Head weight had only minor effects on nutrient concentrations, but total accumulation increased with head size. Some cultivars had nearly twice the accumulation of nutrients as others. This work suggests that cultivars can be selected for production of nutrient-rich lettuce. 相似文献
Investigations on porosity and pedological features were carried out on thin sections of samples of a clay soil treated with a ferric conditioner. The effect of wetting-drying cycles was considered and also surface shrinkage was determined. Micromorphometric determinations of porosity, pore size distribution and number of pores per mm2 were carried out by a Leitz-Classimat apparatus. Pore shape and pedological features of ferric compounds were analysed by the point-count method. Surface shrinkage data show great differences between treated and control samples at the first wetting-drying cycle but similar values at the end of the experiment. The statistical processing of micromorphometric data shows significant differences between the control and treated soil material. Wetting-drying cycles influence the number of pores and porosity mainly in the treated soil samples. The pore size distribution is more homogeneously represented in all size classes within treated samples. Also the statistical processing of data of pore shapes and pedological features shows significant differences between control and treated soil samples. Only planar pores are not influenced by the treatment. The wetting-drying cycles affect neither the pore shape, except for planar pores, nor the different pedological features. 相似文献
Tomato plants (Lycopersicum esculentum Mill, ‘Red Cherry Small’), grown in 15 cm diameter plastic pots with a standard greenhouse medium (1:1:1, by volume, soil:peat:sand) were irrigated for 15 weeks with liquid sewage sludge containing a liquid cationic conditioner (Petroset SB, Phillips Petroleum Company, Bartlesville, Oklahoma) to determine the effect of the conditioner on Cd and Zn availability. Half of the plants received 50 ml week?1 liquid digested sludge with no conditioner and half of the plants received 50 ml week?1 sludge containing 0.25 ml conditioner (200:1, by volume, sludge:conditioner). Plant height was measured weekly. Plants were harvested 3, 6, 9, 12, and 15 weeks after sludge treatments began and separated into roots, shoots, and fruits for dry weight determination and Cd and Zn analyses. Soil and sludge crusts were sampled at the same times and analyzed for extractable concentrations of Cd and Zn. Dry weights of plants grown with conditioned sludge were similar to those grown with nonconditioned sludge. Plants with conditioner flowered and fruited one and two weeks earlier, respectively, than plants without conditioned. Six weeks after treatments began, when the plants had grown to their greatest height, Cd concentrations in sludge crusts, soil, and roots receiving conditioner were 2.0, 1.5, and 2.1 times greater, respectively, than crusts, soil and roots not receiving conditioner. After the six weeks sampling time, Cd concentrations in crusts, soil, and roots receiving conditioned sludge were similar to those in crusts, soil, and roots receiving nonconditioned sludge. At the third-week sampling time, shoots of plants grown with conditioner had 2.6 times more Cd than shoots of plants grown without conditioner. Cadmium concentrations in shoots from both treatments were similar at later sampling dates. Cadmium content of fruits was the same for both treatments all sampling times. Zinc content of roots, shoots, fruits soil, and sludge crusts was no affected by the conditioner. Results showed that a cationic conditioner, added to sludge, increased the availability of Cd, but not of zn, for tomato plants until maximum height was reached. 相似文献