通过纯培养蛋白质组学跟踪研究石油污染的土壤上微生物群落的变化

Hydrocarbon contamination may affect the soil microbial community, in terms of both diversity and function. A laboratory experiment was set-up, with a semi-arid control soil and the same soil but artificially contaminated with diesel oil, to follow changes in the dominant species of the microbial community in the hydrocarbon-polluted soil via proteomics. Analysis of the proteins extracted from enriched cultures growing in Luria-Bertani (LB) media showed a change in the microbial community. The majority of the proteins were related to glycolysis pathways, structural or protein synthesis. The results showed a relative increase in the complexity of the soil microbial community with hydrocarbon contamination, especially after 15 days of incubation. Species such as Ralstonia solanacearum, Synechococcus elongatus and different Clostridium sp. were adapted to contamination, not appearing in the control soil, although Bacillus sp. dominated the growing in LB in any of the treatments. We conclude that the identification of microbial species in soil extracts by culture-dependent proteomics is able to partially explain the changes in the diversity of the soil microbial community in hydrocarbon polluted semi-arid soils, but this information is much more limited than that provided by molecular methods.     

施入粉煤灰和污泥对酸性淋溶土镉和铅吸附的影响

The safe recycling of fly ash (FA) and sewage sludge (SS) in the agricultural processes comprises an important environmental technology on waste management. Soils amended with FA and SS may change their ability to adsorb heavy metals due to either increase of soil pH or decomposition of sludge-borne organic matter. Thus, Cd and Pb sorption was investigated by 1-month incubation under soil moisture content at field capacity and room temperature with an acidic Typic Haploxeroalf from central Greece amended with varying amounts of FA and SS. Batch experiments were conducted by equilibrating the soil samples with CaCl₂ solutions containing 0-400 mg Pb L^-1 or 0-100 mg Cd L^-1. The results showed that the Freundlich equation described well the Cd and Pb sorption. Distribution coefficient (K_d) values of Pb were higher than those of Cd in all the treatments of this study. Application of FA increased K_d values for Cd and Pb to 8.2 and 2.3 times more than the controls, respectively. Simultaneous applications of FA and SS caused a K_d increase of 3.8 and 2.1 times compared to the treatments that received only SS for Cd and Pb, respectively. Treatment of SS alone did not significantly change Cd and Pb sorption compared to the controls. The sorption reactions seemed to be mainly affected by soil pH, which was revealed by the significant correlations of Cd and Pb sorption with soil pH. These suggested that fly ash was very useful as a low-cost adsorbent for Cd and Pb and could be used as an ameliorant for biosolid-amended acidic soils.     

北约旦地区降水侵蚀因子的近似估算研究

Despite being in arid and semi-arid areas, erosion is largely a result of infrequent but heavy rainfall events; therefore, rainfall erosivity data can be used as an indicator of potential erosion risks. The purpose of this study was to investigate the spatial distribution of annual rainfall erosivity in North Jordan. A simplified procedure was used to correlate erosivity factor R values in both the universal soil loss equation (USLE) and the revised universal soil loss equation (RUSLE) with annual rainfall amount or modified Fournier index (F_mod). Pluviometric data recorded at 18 weather stations covering North Jordan were used to predict R values. The annual values of erosivity ranged between 86-779 MJ mm ha^-1 h^-1 year^-1. The northwest regions of Jordan showed the highest annual erosivity values, while the northeastern regions showed the lowest annual erosivity values.     

pH对土壤重金属吸附动力学的影响

The pH effect on the sorption kinetics of heavy metals in soils was studied using a constant flow leaching method. The soil samples were red soil collected from Yingtan, Jiangxi, and yellow-brown soil from Nanjing, Jiangsu. The heavy metals tested were zinc and cadmium. Assuming that the experimental data fitted to the following kinetic rate equation: 1/c·dx/dt = kx_∞-kx, the rate constant k of sorption could be determined from the slope of the straight line by plotting of 1/c·dx/dt vs. x. The results showed that the pH effect on the rate constants of heavy mental sorption in soils was very significant. The values of k decreased with increasing pH. The sorptions were more sensitive to pH in red soil than in yellow-brown soil.     

蚯蚓对不同分解阶段有机质的响应

This study was conducted to examine the responses of earthworms to soil organic matter and litter at different decomposition stages and their contributions in litter decomposition processes in southern subtropical areas of China. Two plantations were selected as the study sites: Site Ⅰ was dominated by the exotic endogeic earthworm species Ocnerodrilus occidentalis; Site Ⅱ was dominated by epigeic species Amynthas corticis. After the fallen litter and earthworms were removed or expelled, four treatments were set up as: reserving the top soil (0-5 cm, equal to H layer) (H), removing the top soil and adding fresh litter (Le), removing the top soil and adding semi-decomposed litter (Li), and a control with no top soil nor any litter (CK). Five randomized blocks that were enclosed with nylon nets on the top were set up in each site, and then the four treatments were arranged randomly in each block. After 2-3 months, earthworms were collected using the formalin method. The results showed that Ocnerodrilus occidentalis preferred Treatment H though it was found in Treatments Le and Li as well; Amynthas corticis preferred Treatment Li though sometimes it also appeared in Treatment H; and Amynthas sp., another epigeic species, was mainly present under Treatment Le and only appeared in Treatment H occasionally. These findings confirmed that earthworm species belonging to different ecological groups had different responses to organic matter at different decomposition stages. The impacts of earthworm communities dominated by O.occidentalis mainly appeared at the later periods of litter decomposition.     

Relationship between granitic soil particle-size distribution and shrinkage properties based on multifractal method

The mechanical properties of granitic residual soils vary with depth due to changes in soil type and heterogeneity caused by weathering. The purpose of this study was to relate the spatial variation of particle-size distribution (PSD) of granitic soils with soil shrinkage parameters using multifractal theory. The heterogeneity of PSD and pedogenic processes were depicted in detail by multifractal dimensions. The PSD generally increased with the increase of profile depth in accordance with the variation of single fractal dimension (D) ranging from 2.45 to 2.65. The shrinkage limit was greatly influenced by the multifractal dimension parameters, including information dimension (D₁) and capacity dimension (D₀) (Adjusted R²=0.998, P < 0.01), and the maximum linear extensibility (κ_v) was determined by spectral width (△α) and bulk density, with the latter explaining 89% of the total variance of κ_v (P < 0.01). Soil shrinkage characteristic curve was fitted by the modified logistic model (R² > 0.97, root sum of squares < 0.1), and the water variation corresponding to the maximum change rate of linear extensibility was determined by the silt content (R²=0.81, P < 0.01). Overall, the shrinkage of granitic soils was primarily influenced by PSD and soil compactness.     

应用反射光谱法估测矿区附近农田土壤As, Cu污染

Concentrations of Iron (Fe), As, and Cu in soil samples from the fields near the Baoshan Mine in Hunan Province, China, were analyzed and soil spectral reflectance was measured with an ASD FieldSpec FR spectroradiometer (Analytical Spectral Devices, Inc., USA) under laboratory condition. Partial least square regression (PLSR) models were constructed for predicting soil metal concentrations. The data pre-processing methods, first and second derivatives (FD and SD), baseline correction (BC), standard normal variate (SNV), multiplicative scatter correction (MSC), and continuum removal (CR), were used for the spectral reflectance data pretreatments. Then, the prediction results were evaluated by relative root mean square error (RRMSE) and coefficients of determination (R²). According to the criteria of minimal RRMSE and maximal R², the PLSR models with the FD pretreatment (RRMSE = 0.24, R² = 0.61), SNV pretreatment (RRMSE = 0.08, R² = 0.78), and BC-pretreatment (RRMSE = 0.20, R² = 0.41) were considered as the final models for predicting As, Fe, and Cu, respectively. Wavebands at around 460, 1 400, 1 900, and 2 200 nm were selected as important spectral variables to construct final models. In conclusion, concentrations of heavy metals in contaminated soils could be indirectly assessed by soil spectra according to the correlation between the spectrally featureless components and Fe; therefore, spectral reflectance would be an alternative tool for monitoring soil heavy metals contamination.     

Changes in soil free-living diazotrophic community and co-occurrence patterns along desert wetland degradation gradient in the Mu Us Desert, northern China

Climate change and human activity have led to the degradation of desert wetlands. Free-living diazotrophs are vital for soil nitrogen input. However, a comprehensive understanding of how soil free-living diazotrophic communities and their co-occurrence patterns respond to desert wetland degradation is lacking. Here, quantitative polymerase chain reaction (qPCR), amplicon sequencing targeting nitrogenase gene (nifH), and network analysis were used to investigate the abundance, diversity, community composition, and co-occurrence patterns of soil free-living diazotrophs along the wetland degradation gradient, i.e., non-degraded (ND), lightly degraded (LD), moderately degraded (MD), and severely degraded (SD), in the southeastern Mu Us Desert, northern China. The abundance and Shannon, Simpson, Chao 1, and ACE indexes decreased (P < 0.05) by 14.6%, 20.7%, 2.1%, 46.5%, and 45.0%, respectively, in SD wetland, whereas no significant difference (P > 0.05) was observed between ND and LD wetlands. The relative abundance of Proteobacteria generally decreased (by 53.5%–19.7%) across the different degradation levels, while the relative abundance of Cyanobacteria increased (by 6.2%–40.1%) from ND to MD levels. The abundance, diversity, and community composition of diazotrophs were most strongly related to soil organic carbon, followed by total nitrogen, moisture, and pH. The least number of network nodes and edges and the lowest density were observed for MD and SD wetlands, indicating that the complexity of free-living diazotrophic networks was reduced by continued degeneration. Overall, severe desert wetland degradation affected the abundance, diversity, and network complexity of soil free-living diazotrophs more negatively than light degradation. This degradation promoted the growth of autotrophic diazotrophs and inhibited the growth of heterotrophic diazotrophs. These changes were mostly related to the loss of soil organic carbon.     

根迹土壤根诱导的化学变化对植物吸收重金属的影响

It is increasingly recognized that metal bioavailability is a better indicator of the potential for phytoremediation than the total metal concentration in soils; therefore, an understanding of the inffuence of phytoremediation plants on metal dynamics at the soil-root interface is increasingly vital for the successful implementation of this remediation technique. In this study, we investigated the heavy metal and soil solution chemical changes at field moisture, after growth of either Indian mustard (Brassica juncea) or sunffower (Helianthus annuus L.), in long-term contaminated soils and the subsequent metal uptake by the selected plants. In addition, the fractions of free metal ions in soil solution were determined using the Donnan membrane technique. After plant growth soil solution pH increased by 0.2-1.4 units and dissolved organic carbon (DOC) increased by 1-99 mg L^-1 in all soils examined. Soluble Cd and Zn decreased after Indian mustard growth in all soils examined, and this was attributed to increases in soil solution pH (by 0.9 units) after plant growth. Concentrations of soluble Cu and Pb decreased in acidic soils but increased in alkaline soils. This discrepancy was likely due to a competitive effect between plant-induced pH and DOC changes on the magnitude of metal solubility. The fractions of free Cd and Zn ranged from 7.2% to 32% and 6.4% to 73%, respectively, and they generally decreased as pH and DOC increased after plant growth. Metal uptake by plants was dependant on the soil solution metal concentration, which was governed by changes in pH and DOC induced by plant exudates, rather than on the total metal concentrations. Although plant uptake also varied with metal and soil types, overall soluble metal concentrations in the rhizosphere were mainly inffuenced by root-induced changes in pH and DOC which subsequently affected the metal uptake by plants.     

酸性农田土壤镉污染修复钝化材料筛选研究

[目的]研究0.3 mg kg-1、1.0mg kg-1、1.5 mg kg-1三种不同镉污染水平的酸性农田土壤单一或复配添加海泡石(H)、膨润土(P)、钙镁磷肥(G)、磷矿粉(L)四种钝化剂钝化镉污染的效果.[方法]采用室内培养模拟实验,添加单一纯化剂处理于开始培养后10 d、20 d、30 d,复配添加钝化剂处理于...     

淹水条件下含硫锌肥与蒜皮对镉生物有效性及水稻产量的影响

采用盆栽试验,研究了淹水条件下施用锌肥(ZnSO4.7H2O)与含巯基废弃物(蒜皮)对污染土壤中镉生物有效性的影响。结果表明,与对照相比,施用锌肥(0.2 g kg-1)后水稻增产25%(P<0.05),在淹水平衡7 d时土壤中有效硫和有效锌含量显著提高,增幅分别为267.9%和684.4%,而土壤中有效态镉含量降幅达61.3%(P<0.05);水稻移栽30 d和60 d时,土壤中有效硫和有效锌含量仍显著高于对照,有效态镉显著低于对照,但随着时间的推移均呈下降趋势,水稻根系和糙米镉含量较对照降低了31.0%(P<0.05)和38.9%(P<0.05)。与对照相比,施用蒜皮(1 g kg-1)的土壤有效硫随时间的推移呈上升趋势,同时有效态镉含量下降,水稻根系和糙米中镉含量降低,但差异均不显著。锌肥与蒜皮配合施用的效果优于两者单施。因此,淹水还原条件下施用适量含硫锌肥可有效降低污染土壤中镉的活性,减少水稻的镉累积,而本试验条件下施用富含巯基的蒜皮效果不明显。     

生物炭与沸石混施对不同污染土壤镉形态转化的影响

采用室内培养模拟了低(1.0 mg/kg)、高(10 mg/kg)镉污染的土壤,通过向镉污染土壤中添加0.4%,2%,10%的1∶1的生物炭和沸石的混合物,探究了生物炭及沸石混施对不同程度镉污染土壤的pH和镉形态变化的影响。结果表明:2种不同程度镉污染土壤的pH均较CK有所提高,且随钝化剂用量的增加而增大。随着培养时间的延长,低污染土壤pH呈现降低趋势,而高污染土壤pH先升高后降低最后趋于稳定。培养后期,低污染和高污染土壤在混合物添加量分别为2%和10%时有效态镉降低比例最大,降低比例分别为56.78%和27.33%。各处理土壤随生物炭和沸石混合物添加量的增加交换态镉降低比例逐渐增大,培养后期,低污染土壤的交换态镉较CK分别降低8.35%,13.81%,20.65%,高污染土壤的交换态镉较CK分别降低10.02%,22.34%,33.01%。各处理的钝化剂能够明显的降低交换态镉的含量,增加碳酸盐结合态、铁锰氧化物结合态、有机结合态和残渣态镉的含量,低污染土壤的有机结合态明显高于高污染土壤。由此可见,生物炭与沸石混施能够降低土壤重金属的生物有效性,为农田土壤修复奠定了理论基础。     

不同改良剂对土壤-叶菜系统Cd迁移累积的调控作用

为筛选适合在中轻度镉污染土壤上有效降低叶菜吸收镉的改良剂及用量,采用镉污染菜地土壤进行盆栽试验,研究不同用量的石灰、泥炭和碱渣对小白菜（Brassica chinensis L.）生物量、镉吸收量,土壤pH及有效态镉含量的影响。结果表明,3种改良剂对小白菜生长均无显著的抑制作用;与不施改良剂的处理相比,石灰、泥炭显著抑制小白菜对镉的吸收,地上部镉含量与石灰和泥炭用量均呈显著负相关关系（R=-0.668、-0.785,P〈0.05）,碱渣对小白菜地上部镉含量的影响不显著,但显著增加根系镉含量;改良剂均显著提高土壤pH,但对DTPA-Cd影响不同,石灰显著降低DTPA-Cd,泥炭、碱渣均有增加DTPA-Cd含量的趋势;泥炭对土壤-小白菜系统Cd迁移的调控效果最佳,其最佳用量为20 g.kg-1土,石灰次之,碱渣不适合。     

改良剂对镉污染酸性水稻土的修复效应与机理研究

为探明田间条件下施用石灰、钙镁磷肥、海泡石和腐殖酸等改良剂对Cd污染酸性水稻土的修复效应和作用机理, 通过在Cd污染区建立田间小区试验, 研究了改良剂单施和与石灰配施对Cd污染酸性水稻土中Cd作物有效性的影响。结果表明, 施用改良剂有效地改变了土壤中Cd的存在形态, 除腐殖酸外, 其他改良剂均使土壤酸提取态Cd不同程度地转化为可还原态Cd和残渣态Cd; 施用改良剂可使0.1 mol·L^-1 NaNO₃和 0.01 mol·L^-1CaCl₂提取态Cd 降低26%~97%, 降低效果为石灰+海泡石>海泡石>石灰+钙镁磷肥>钙镁磷肥>石灰>石灰+腐殖酸>腐殖酸; 改良剂使水稻地上部分的Cd吸收量降低6%~49%。试验结果还显示, 施用改良剂提高土壤pH是引起土壤中Cd作物有效性降低的主要原因之一。根据田间试验的结果, 海泡石可推荐作为Cd污染酸性水稻土的改良剂, 而腐殖酸则不宜使用。     

生物炭与沸石复配对碱性土壤铅镉有效性的影响

【目的】以生物炭单施及其与沸石复配为钝化剂,研究其对铅镉复合污染碱性土壤理化性质及铅镉有效性的影响,以期用钝化技术为碱性土壤重金属污染原位修复提供理论和实践支持。【方法】以河南某金属冶炼厂附近铅(Pb)镉(Cd)污染的碱性菜地土壤(Pb 227.75 mg kg^-1、Cd 3.38 mg kg^-1)为研究对象,采用盆栽试验,研究生物炭单施及其与沸石复配(生物炭∶沸石=1∶1)不同施入量(0、1%、2.5%、5%)对土壤理化性质、土壤Pb、Cd有效态含量、青菜根和叶中Pb、Cd含量以及青菜富集转运Pb、Cd的影响。【结果】与对照相比,生物炭单施及其与沸石复配处理,使土壤pH提高了0.03～0.17个单位,与对照无显著差异,但显著提高了土壤有机质、碱解氮、有效磷和速效钾含量(P <0.05)。土壤有效态Pb、Cd含量随钝化剂施用量增加呈下降趋势,分别下降了10.69%～32.75%和7.63%～26.72%,相同施用量下复配处理效果优于单施处理。生物炭及其复配沸石促进了青菜生长,降低了青菜Pb的含量,根部和茎叶中Pb的含量比对照分别下降了2...     

八宝景天–柑橘间作降低柑橘根际土壤镉含量以减少对镉的吸收

  【目的】  超富集植物与经济作物间作是实现重金属污染农田边生产边修复的有效措施。为此，研究八宝景天 (Hylotelephium spectabile) 和柑橘间作对柑橘重金属吸收累积的影响，为柑橘生产提供安全、经济有效的栽培措施。  【方法】  以早熟和晚熟柑橘、八宝景天为试材进行盆栽试验，以全Cd含量为0.92 mg/kg的污染土壤和0.06 mg/kg的清洁土壤为供试土壤。分别设置早熟和晚熟柑橘单作、八宝景天单作、早熟和晚熟柑橘–八宝景天间作和柑橘–八宝景天限制性间作，共7个处理，限制性间作采用半透膜根际袋将八宝景天和柑橘根系分开。在植株生长74天 (7月) 和218天 (12月)时采样，调查植株生物量和Cd含量，分别测定根际土壤全Cd和有效态Cd含量。  【结果】  与柑橘单作相比，与八宝景天间作柑橘的叶片Cd含量降低了26.7%，与清洁土壤种植的柑橘叶片Cd含量 (0.011 mg/kg) 相近。间作条件下，柑橘根际土壤中全Cd含量由0.92 mg/kg降低至0.75 mg/kg，有效态Cd含量由单作处理的0.82 mg/kg降低至0.78 mg/kg，低于柑橘单作处理；柑橘–八宝景天间作柑橘根际土壤中全Cd的减少量是柑橘–八宝景天限制性间作柑橘根际土壤全Cd减少量 (6.52%) 的2.83倍。柑橘–八宝景天间作中八宝景天对土壤Cd的年提取量、年去除率分别达1.40 mg/pot、3.34%，与其单作 (1.50 mg/pot、3.73%) 相比，去除效率降低了10.6%，其主要原因是间作降低了八宝景天的生物量。  【结论】  尽管柑橘–八宝景天间作影响八宝景天对镉的去除效率，但显著降低了柑橘根际全Cd和有效态Cd含量，进而将柑橘叶片Cd含量降低到与清洁土壤下近似的水平，实现了边修复边安全生产的目标，因此，柑橘–八宝景天间作可作为中低度Cd污染农田土壤修复的重要生物措施。     

水分管理和施用石灰对水稻镉吸收与运移的影响

通过田间试验,研究了间歇灌溉和全生育期淹水2种水分管理结合水稻分蘖期施用石灰对不同水稻生育期的土壤和水稻各组织中Cd分布与运移的影响。研究结果表明,全生育淹水和施用石灰均能升高土壤p H值,降低土壤中有效态Cd含量;施用石灰能降低土壤中酸可提取态Cd所占比例而残渣态所占比例增加。在全生育期淹水条件下施用石灰有利于改善土壤性状并提高土壤中Fe质量百分含量。与不施用石灰相比,在间歇灌溉条件下,施用石灰处理的糙米中Cd质量分数从0.86 mg/kg降低到0.56 mg/kg,而在全生育期淹水条件下,施用石灰处理的糙米中Cd质量分数从0.77 mg/kg降低到0.34 mg/kg;无论间歇灌溉还是全淹水处理条件下,施用石灰均增加了水稻总生物量。施用石灰后,在灌浆期,水稻茎叶中Cd的富集系数显著降低(P0.05);在成熟期,根和稻米中Cd的富集系数显著降低(P0.05);在全生育期淹水条件下,成熟期水稻根到茎叶转运系数和茎叶到米中转运系数均显著降低(P0.05)。水稻糙米中Cd含量与土壤中有效态Cd含量、水稻地上部Cd累积量呈显著正相关,与土壤p H值呈显著负相关。上述研究结果表明,施用石灰能够显著降低稻田土壤中Cd的生物有效性;采用全生育期淹水结合在分蘖期施用石灰是降低稻米中Cd含量有效措施且不会导致水稻减产。     

干湿交替下生物炭对复合污染土壤中镉砷有效性的影响

为了明确活性炭工业的副产品——杏壳生物炭和水分管理模式对石灰性土壤重金属有效性的钝化效果,采用重度Cd、As复合污染的农田土壤,通过土壤培养方法探索了干湿交替水分管理模式下,添加不同用量生物炭对土壤中Cd、As有效性的影响。结果表明:从土壤溶液中Cd、As浓度的变化来看,干湿交替培养条件下,添加2%~10%生物炭处理的土壤溶液中Cd浓度均显著低于对照(P<0.05),降幅为33.1%~62.2%,说明干湿交替模式下添加生物炭显著促进了Cd由土壤液相向土壤固相的转移,而添加生物炭对土壤溶液中砷浓度的影响不稳定,其主要受土壤水分管理模式的影响;从土壤固相Cd、As提取态的变化来看,添加生物炭(6%,8%,10%)处理与CK相比,可显著降低土壤中DTPA提取态Cd和NH4H2PO4提取态As的含量(P<0.05),降幅分别为8.7%~16.8%,5.1%~7.9%,表明干湿交替下添加生物炭显著降低了土壤Cd、As有效性;土壤连续分级提取的结果显示,施用生物炭促进了土壤Cd由酸可提取态和可氧化态向残渣态转化,土壤As由专性吸附态和无定形—弱结晶铁铝或铁锰水化氧化物结合态向残渣态转化,显著降低了污染土壤Cd、As活性。因此,在重度Cd、As复合污染的石灰性土壤区,施用6%生物炭并保持干湿交替的水分管理模式能显著降低土壤镉砷的有效性。     

Relations Between Soil Properties and Selected Heavy Metal Concentrations in Spring Wheat (Triticum aestivum L.) Grown in Contaminated Soils

Spring wheat was grown in soils near a non-ferrous metals mining and smelting base in Baiyin city, Gansu province, P.R. China. The area studied is 501 km². Some of the croplandshad been contaminated by heavy metals mainly through wastewaterirrigation or aerial deposition. The soil samples were analyzedfor pH, organic matter and available phosphorous (P); also fortotal cadmium (Cd), lead (Pb), copper (Cu) and zinc (Zn) contents. Spring wheat grains were also analyzed for heavy metals. The results were interpreted using multiple linear correlation and stepwise regression analyses. The increment oftotal soil contents of selected heavy metals could enhance grain Cd accumulation, and the increment of total Zn content of soil could lower the grain Pb accumulation. The correlationswere markedly increased by including other soil properties forgrain Cd and Pb. Stepwise regression analyses indicated that the effect of soil pH and available P on the uptake of grain Cd were greater than that of the other total soil contents ofheavy metals. Grain Cd and Pb could be reliably predicted bythe total soil contents of Cd and Pb while the uptake of grainZn and Cu were not satisfactorily predicted.