不同锌浓度有机肥对土壤酶活性及微生物数量的影响

采用室内培养方法,探究了含不同质量浓度(600、1 200、1 800mg/kg)锌的有机肥对土壤酶活性及微生物的影响。结果表明:(1)在整个培养阶段,含锌的有机肥总体显著抑制土壤脲酶、蔗糖酶、脱氢酶和过氧化氢酶活性,对碱性磷酸酶活性影响不显著;随着有机肥中锌浓度的增大,脲酶、脱氢酶、蔗糖酶活性总体显著降低。(2)整个培养阶段,含1 800mg/kg锌的有机肥促进土壤中真菌增长;对土壤中细菌总体也有促进作用;对土壤中放线菌呈先抑制后激活的作用,最后趋于稳定。     

改良剂对土壤Cu形态转化及其生物可给性的影响

通过室内土壤培养实验,研究添加9种不同改良剂(沸石、石灰、磷矿粉、油菜秸秆、堆肥、赤泥、生物调理剂、生物炭和骨炭)对污染土壤Cu化学形态和生物可给性的影响。培养2个月,除堆肥处理外,添加5%的其他8种改良剂均显著地提高了土壤的p H值,提高效果为石灰生物炭赤泥生物调理剂油菜秸秆=骨炭磷矿粉沸石。培养2个月后,添加所有改良剂均显著地降低了土壤中酸可提取态Cu的含量,生物调理剂、生物炭和骨炭处理效果最为显著,分别比对照下降28%、18.1%和33.7%。添加不同的改良剂对土壤Cu的生物可给性也有影响。培养1个月,石灰、生物炭和骨炭处理分别导致土壤中生物可给性Cu含量比对照降低9.8%、10.5%和18.3%;培养2个月,赤泥、生物炭和堆肥处理分别导致生物可给性Cu含量比对照降低13.2%、17.6%和18.6%。研究表明,生物炭和骨炭可作为Cu污染土壤的理想改良剂。     

香菇菌渣对土壤微生态的影响

为研究香菇菌渣添加对土壤质量改善的效果和机制,在土壤中添加质量分数为0(对照)、1.5％、3.0％、4.5％的香菇菌渣进行培养处理,并定期检测土壤中各类微生物的数量与某些酶活性.结果表明:添加香菇菌渣对土壤微生物数量和酶活性都有不同程度的提高作用,其中真菌数量、放线菌数量、几丁质酶活性和脱氢酶活性均随添加量的增加而增大,说明香菇菌渣能够增加土壤中微生物群落的规模,从根本上有利于土壤质量的改善,同时还增强了土壤潜在的抑病能力；4.5％处理的平均真菌数量、放线菌数量、几丁质酶活性、脱氢酶活性分别为对照的1 399.00％、2 773.33％、1 309.36％、2 512.29％.     

化学预氧化-生物强化-生物刺激对土壤中菲降解的联合效应

通过室内实验,探究了低浓度过硫酸盐预氧化耦合生物强化或生物刺激技术处理下土壤中菲的降解率和修复效应。结果表明,浓度为0.1 mmol·g~(-1)、温度为50℃热活化的过硫酸钠对土壤中菲7 d的降解率为22.7%。预氧化后,加入高效降解菌和营养物质,强化微生物对菲的降解,继续培育21 d,最终降解率较第7天可提高8.08%～18.59%。同时添加高效降解菌和营养物质N,对土壤中菲的降解促进作用最强,最终降解率可达41.29%,较仅进行化学氧化的对照组和仅进行微生物降解的对照组分别提高17.44%和22.86%,较预氧化后不进行微生物强化的对照组提高12.9%。降解期间,土壤微生物数量和pH呈先下降,后上升趋势,最终维持在相对稳定水平。相关性分析结果表明,土壤中菲的降解率与氧化剂和营养物质N的添加呈显著正相关,土壤微生物数量与pH呈正相关,与氧化剂呈负相关,土壤pH与氧化剂及营养物质P呈负相关。研究结果证实了化学预氧化耦合生物强化和生物刺激技术能有效促进微生物对菲污染土壤的修复。     

污泥蛋白肽对土壤微生态及植物生长调控

以污泥为原料制备平均分子量为5 000道尔顿以内的蛋白肽,并以有机肥、复合肥和尿素为对照,研究蛋白肽对土壤微生物种群数量、土壤酶活性以及对所种植的十字花科植物红菜薹的生理指标影响效应,结果表明,在施加相同含氮量(0.1 g N)的条件下,污泥蛋白肽实验组的土壤微生物种群数量最高,达到39.28×107个/g,比最低的尿素实验组(10.38×107个/g)高73.6%;在对土壤酶活方面,污泥蛋白肽实验组的脲酶活性比所有对照组高,达到9.82 mg/(g·h),最低是复合肥实验组,其脲酶活性为6.54 mg/(g·h);利用蛋白肽所种植红菜薹的生物量分别是有机肥、复合肥和尿素的14.1倍、8倍和3.1倍,并且通过计算所施氮量与植株总氮量的比值——氮转化率,得出蛋白肽所种植红菜薹植株的氮转化率达到222.3%。这进一步表明蛋白肽是一种植物速效并且高效肥料。     

采煤沉陷区耕地土壤微生物数量及酶活性的空间特征

通过野外调查和采样分析,研究了焦作矿区韩王矿沉陷区不同沉陷部位和不同深度耕地的土壤微生物数量及酶活性特征。研究结果表明:与对照区比较,沉陷区耕地土壤微生物数量、酶活性赋存特征及微生物类群组成比例发生了明显变化。沉陷区表层(0~5 cm)、上层(5~10 cm)、中层(10~20 cm)土壤微生物总数、细菌数量均明显减少,而下层(20~40 cm)土壤微生物总数、细菌、真菌、放线菌数量均明显升高。沉陷区表层、上层土壤细菌数量所占微生物总数比例分别降低了20.64%和13.17%,而放线菌数量所占比例分别升高了20.69%和12.66%。沉陷区表层土壤脲酶、蔗糖酶、磷酸酶、脱氢酶、过氧化氢酶和多酚氧化酶活性分别降低了1.5%、17.5%、22.0%、35.3%、20.4%和5.4%。不同沉陷部位的土壤微生物数量及部分酶活性指标空间异质性显著(p0.05)。沉陷区土壤真菌、放线菌数量、蔗糖酶、磷酸酶、脱氢酶、过氧化氢酶、多酚氧化酶活性较对照区均具有不同的垂向分布特征。表明采煤引发的地表沉陷使耕地土壤微生物数量及酶活性在水平和垂直方向上均发生了显著变化,而这些变化是导致沉陷区耕地退化、生产力降低的重要原因。     

生物处理镉污染土壤及其酶活性研究

以添加镉的天津农田土壤为对象,分别设定空白处理、添加诺沃肥处理及生物强化处理(添加1株紫外线诱变工程菌和诺沃肥).研究土壤在不同pH、温度和含水率条件下可提取有效态镉(E-Cd)、过氧化氢酶及脲酶活性的变化情况.结果表明,添加诺沃肥处理可以有效降低E-Cd含量.而生物强化处理可进一步促进镉的固定效果;最适合生物修复的环境条件为PH 7.0、温度30℃和土壤含水率50%;添加诺沃肥处理和生物强化处理的土壤中过氧化氢酶和脲酶活性明显高于空白处理,说明生物修复后,土壤酶活性已经恢复,表明这2种处理能改善土壤结构和性能,提高土壤的肥力.     

底泥修复中温度对微生物活性和污染物释放的影响

通过分析底泥中微生物的酶活性以及污染物的释放规律,探讨了温度对河道底泥生物修复的影响.结果表明,底泥中微生物的脱氢酶、脲酶和磷酸酶的活性随着温度的升高而显著增大,但温度对纤维素酶的活性影响较小.4 ℃和10 ℃时底泥中污染物的释放量和微生物的酶活性均较低,水质较稳定;20～37 ℃时底泥中污染物的释放量明显增加,微生物的新陈代谢能力有较大提高,水体的自净能力较强.在各种因素的综合作用下,20～30 ℃是进行底泥生物修复的适宜环境温度.此外,当pH为9.0以及添加葡萄糖时,底泥中微生物均表现出较高的脱氢酶活性.     

矿化垃圾中的微生物区系与酶活性变化特征研究

选择某市郊城市生活垃圾填埋场为研究对象,对填埋时间分别达6、8、10年的矿化垃圾中的微生物区系与酶活性变化特征进行了比较。结果表明,表层(0～50 cm)和底层(100～150 cm)矿化垃圾中的微生物数量和酶活性变化幅度大于中层(50～100cm);填埋达6、8、10年后的各层矿化垃圾中的细菌数量明显低于对照,放线菌数量则明显高于对照,而真菌数量在表层和中层中高于对照或与对照相当,在底层则低于对照,各层中的脲酶、碱性磷酸酶、碱性磷酸酶活性则明显高于对照或与对照相当;总体来说,相同填埋深度的矿化垃圾中,填埋达6～8年的细菌、真菌、放线菌数量和脲酶、碱性磷酸酶、酸性磷酸酶活性的变化幅度要大于填埋8～10年的,且均在填埋8～10年趋于稳定。     

生物有机肥在土壤改良和重金属污染修复中的研究进展

生物有机肥兼具有机肥料和微生物肥料的性质,可以培肥土壤、调控土壤微生态平衡、改善农产品品质、控制土壤中重金属的有效性,也是农业废弃物资源化利用的重要手段。综述了生物有机肥的主要特征、生物有机肥在土壤重金属污染中的修复作用,重点介绍了生物有机肥在改良土壤性质和修复重金属方面的优越性能,指出生物有机肥领域当前存在的问题,并提出未来在肥源监管、标准修订和品种研发等方面进行改进,为保障农产品的质量安全、有机肥料的资源化利用提供参考。     

污染土壤的淋洗法修复研究进展

污染土壤淋洗技术是修复污染土壤的一种新方法 ,是对污染土壤生物修复的一种补充 ,使污染土壤修复的系统化成为可能。淋洗法主要使用淋洗剂清洗土壤 ,使土壤中污染物随淋洗剂流出 ,然后对淋洗剂及土壤进行后续处理 ,从而达到修复污染土壤的目的。因为淋洗剂的种类和淋洗方式的不同 ,土壤淋洗法可分为许多种类。土壤淋洗法主要受土壤条件、污染物类型、淋洗剂的种类和运行方式等因素影响。综合考虑多方面因素 ,就有潜力设计出经济高效的土壤淋洗系统。土壤淋洗法有很多优点 ,尽管也存在一些问题 ,但其技术上的优势也是其他方法难以取代的 ,所以有良好的应用前景。     

Decontamination of electronic waste-polluted soil by ultrasound-assisted soil washing

Laboratorial scale experiments were performed to evaluate the efficacy of a washing process using the combination of methyl-β-cyclodextrin (MCD) and tea saponin (TS) for simultaneous desorption of hydrophobic organic contaminants (HOCs) and heavy metals from an electronic waste (e-waste) site. Ultrasonically aided mixing of the field contaminated soil with a combination of MCD and TS solutions simultaneously mobilizes most of polybrominated diphenyl ethers (PBDEs), polychlorinated biphenyls (PCBs), polycyclic aromatic hydrocarbons (PAHs), and the analyte metal (Pb, Cu, and Ni) burdens. It is found that 15 g/L MCD and 10 g/L TS is an efficient reagent combination reconciling extraction performance and reagent costs. Under these conditions, the removal efficiencies of HOCs and heavy metals are 93.5 and 91.2 %, respectively, after 2 cycles of 60-min ultrasound-assisted washing cycles. By contrast, 86.3 % of HOCs and 88.4 % of metals are removed from the soil in the absence of ultrasound after 3 cycles of 120-min washing. The ultrasound-assisted soil washing could generate high removal efficiency and decrease the operating time significantly. Finally, the feasibility of regenerating and reusing the spent washing solution in extracting pollutants from the soil is also demonstrated. By application of this integrated technology, it is possible to recycle the washing solution for a purpose to reduce the consumption of surfactant solutions. Collectively, it has provided an effective and economic treatment of e-waste-polluted soil.

     

Axi-symmetric simulation of soil vapor extraction influenced by soil fracturing

Fracturing, either pneumatic or hydraulic, is a method to improve the performance of soil vapor extraction (SVE) in relatively low permeability soils (< 10(-5) cm/s). A two-dimensional model is presented to simulate trichloroethylene (TCE) soil vapor extraction modified by fracturing. Flow and transport is modeled using mobile macropore and micropore networks, which also have been identified in the literature as dual porosity, dual permeability, or heterogeneous flow models. In this model, fluids can flow in both the macropore and micropore networks. This represents a more general model compared to immobile micropore, mobile macropore models presented thus far in the literature for vapor flow and transport in two dimensions. The model considers pressure- and concentration-driven exchange between the macropore and micropore networks, concentration-driven exchange between the gas and sorbed phases within each network, and equilibrium exchange between the gas and water and a sorbed phase within each network. The parameters employed in an example simulation are based on field measurements made at a fractured site. Considered in the simulations were the influence of the volume percentage of fractures, the length of fractures, the relative location of the water table, and the influence of pulsed pumping. For these simulations, internetwork concentration-driven exchange most significantly affected mass removal. The volume percentage of fractures more significantly influence flow and mass removal than the length of fractures. The depth of the water table below the contamination plume only significantly influenced flow and mass removal when the water table was within 60 cm of the bottom of the contaminated soil in the vadose zone for the parameters considered in this study. Pulsed pumping was not found to increase the amount of mass removed in this study.     

Long-term effects of soil heterogeneity on cadmium behaviour in soil

A deterministic model for long-term behaviour of contaminants in the rootzone is developed that includes sorption, leaching, and plant uptake. The model is applied to cadmium accumulation in a sandy soil and uptake of cadmium by barley. Sensitivity analysis showed that the sensitivity of the leaching rate to changes in soil chemical and soil physical parameters decreases as a function of time, and becomes zero when steady state is reached. In contrast, accumulation of cadmium in soil and the plant uptake rate of barley are increasingly sensitive to soil chemical and soil physical parameters as time preceeds. To analyse cadmium behaviour in a field that is heterogeneous with respect to soil physical properties, the interstitial flow velocity was assumed to be a random, lognormally distributed variate. Using Monte Carlo simulation, the average plant uptake rate appeared to be much higher in the stochastic analysis than in the deterministic approach. Steady state is reached after a very long period of time. For a lognormally distributed proton activity, causing heterogeneity with respect to the sorption capacity of the soil, the model predicted similar deviations from the deterministic approach. It is concluded that reference values for groundwater and crop quality are exceeded earlier in a heterogeneous field than in a homogenous soil profile. Moreover, when average values suggest an acceptable situation, variability of the leaching rate and the plant uptake rate can still cause exceedance of reference values in part of the field. Therefore, it is reasoned that environmental quality standards should take soil heterogeneity into account.     

Residual inorganic soil nitrogen in grass and maize on sandy soil

Nitrogen (N) remaining as inorganic ('mineral') soil N at crop harvest (N(minH)) contributes to nitrate leaching. N(minH) data from 20 (grass) and 78 (maize) experiments were examined to identify main determinants of N(minH). N-rate (A) explained 51% (grass) and 34% (maize) of the variance in N(minH). Best models included in addition crop N-offtake (U), offtake in unfertilised plots (U(0)), and N(minH) in unfertilised plots (N(minH,0)) and then explained up to 75% of variance. At low N-rates where apparent N recovery rho keeps to its initial value rho(ini), N(minH) keeps to its base level N(minH,0). At N-rates that exceed the value A(crit) where rho drops below rho(ini), N(minH) rises above N(minH,0) by an amount proportional to (rho(ini)-rho)A. About 80% of (rho(ini)-rho)A was found as N(minH,) in grass as well as in maize. The fraction (1-rho(ini))A does not appear to contribute to N(minH) at low N-rates (A< or =A(crit)) or at high N-rates (A>A(crit)).     

基于客土灌木化技术的弃渣场生态治理

山区公路建设弃渣场常由石渣堆砌而成,其结构松散、孔隙率大、渗透性强,自然生态恢复极为困难.而客土培育技术常用于生态条件恶劣的区域生态治理.以湖北省宜昌某高速公路弃渣场为依托,应用客土灌木化施工工艺,以植被覆盖度和高度作为观测指标,开展了弃渣场生态恢复试验,主要研究灌木生长特点及其对土壤侵蚀的影响,提出适宜宜昌地区弃渣场生态治理的植被类型,对区域内弃渣场生态恢复工程有一定指导意义.     

Differences in herbicide adsorption on soil using several soil ph modification techniques

Abstract

Effects of soil pH on weak acid and weak base herbicide adsorption by soil are often determined by modifying soil pH in the laboratory. Modification of soil pH with acidic or basic amendments such as HCl or NaOH can cause changes in the soil‐solution system that may affect pesticide adsorption. The partition coefficients (K_d) for atrazine and dicamba by Waukegan, Piano, and Walla Walla silt loam soils stabilized in the field at different pH levels were compared to the K_d obtained when the soil pH was adjusted with acidic or basic amendments before herbicide addition. NaOH addition to raise soil pH generally increased the soluble soil organic carbon (SSOC) concentration in solution compared to field soils at the same pH and to soil treated with Ca(OH)₂. NaOH decreased the soil solution ionic strength slightly. Acidifying soils increased the soil solution ionic strength, when compared to field soils at the same pH and had no effect on SSOC concentration. Dicamba adsorption to soil was minimal (K_d < 0.22) and not influenced by soil pH in the range of 4.1 to 6.0; adsorption by laboratory amended soils in some cases underestimated adsorption compared to nonamended soils. Atrazine adsorption increased with decreased pH in all soils, and was overestimated slightly by several laboratory treatments to reduce pH compared to adsorption by field soils. Treatments to raise the pH did not affect atrazine adsorption. Overall, herbicide adsorption differences due to pH modification were small (<30%), and were not affected by soil solution ionic strength, saturating cation, or SSOC concentration in solution.     

Influence of soil moisture on the sequestration of organic compounds in soil

A study was conducted as a part of continuing investigation of the effect of soil moisture on the sequestration of organic compounds aged in the soil. Here, experiments focused on the effects of moisture changes within the soil before, during, and after contaminant addition. The extractability of aged (68 d) phenanthrene was greater from soil that had been subjected to wetting and drying cycles prior to solute addition as compared to soil initially maintained at constant moisture. The recovery of phenanthrene added to moist soil was increased relative to extractability from soil that was air-dried at the time of the contaminant addition. Repeated wetting and drying of soil after the addition of atrazine or phenanthrene resulted in decreased extractability of the compounds as compared to samples maintained at constant moisture. A method for rapidly sequestering contaminants is proposed and may be useful in limiting the time required for laboratory studies involving “aged” contaminants. These data build upon the findings of earlier work from our laboratory and indicate that changes in the moisture conditions of soil can affect the availability of sequestered contaminants possibly through alterations in the structure of the natural solid.     

Effect of sludge-processing mode, soil texture and soil pH on metal mobility in undisturbed soil columns under accelerated loading

The effect of sludge processing (digested dewatered, pelletized, alkaline-stabilized, composted, and incinerated), soil type and initial soil pH on trace metal mobility was examined using undisturbed soil columns. Soils tested were Hudson silt loam (Glossaquic Hapludalf) and Arkport fine sandy loam (Lamellic Hapludalf), at initial pH levels of 5 and 7. Sludges were applied during four accelerated cropping cycles (215 tons/ha cumulative application for dewatered sludge; equivalent rates for other sludges), followed by four post-application cycles. Also examined (with no sludge applications) were Hudson soil columns from a field site that received a heavy loading of sludge in 1978. Romaine (Lactuca sativa) and oats (Avena sativa) were planted in alternate cycles, with oats later replaced by red clover (Trifolium pratense). Soil columns were watered with synthetic acid rainwater, and percolates were analyzed for trace metals (ICP spectroscopy), electrical conductivity and pH. Percolate metal concentrations varied with sludge and soil treatments. Composted sludge and ash had the lowest overall metal mobilities. Dewatered and pelletized sludge had notable leaching of Ni, Cd and Zn in Arkport soils, especially at low pH. Alkaline-stabilized sludge had the widest range of percolate metals (relatively insensitive to soils) including Cu, Ni, B and Mo. Old site column percolate concentrations showed good agreement with previous field data. Little leaching of P was observed in all cases. Cumulative percolate metal losses for all treatments were low relative to total applied metals. Leachate and soil pH were substantially depressed in dewatered and pelletized sludge soil columns and increased for alkaline-stabilized and ash treatments.     

Effect of soil aggregation on the biodegradation of phenanthrene aged in soil

A study was conducted to determine the possible role of soil aggregates in the sequestration of phenanthrene and thus in the declined biodegradation of the hydrocarbon. Phenanthrene aged in Lima loam (2-mm aggregates) showed declined biodegradation with time of aging to the test bacterium P5-2 capable of using sorbed phenanthrene. In contrast, the compound aged in a soil reconstructed with 68% clay-silt and 32% sand that had been separated from the Lima loam was readily mineralized. The percentages of each fraction used were the same as those of the original soil. Biodegradation of aged phenanthrene was not affected significantly by varying the ratios of each fraction in reconstructed mixtures. In experiments with Lima loam, its clay-silt fraction, and its sand fraction, mineralization extent was much lower in soil aggregates compared with the other samples while all had similar organic carbon content of ca. 1.51%. This suggests that aggregation may be another important determinant in the reduced biodegradation of aged phenanthrene.