乙草胺对土壤微生物的影响研究

研究了乙草胺在6种不同浓度下对土壤微生物种群数量及土壤中细菌、放线菌、真菌生长速率的影响。采用密闭法测定乙草胺对土一生物呼吸的影响。结果表明,乙草胺对土壤微生物种群数量及土壤中细菌、放线菌、真菌生长速率均有一定的抑制作用,对土壤微生物呼吸作用具有明显的抑制作用。     

不同土地利用类型土壤微生物群落特征及其影响因素

土壤微生物群落结构特征能够提前反映土壤环境质量的变化,是土壤质量评价的重要因子。为弄清不同土地利用类型土壤微生物群落特征及其影响因素,以内蒙古呼和浩特赛罕区为研究区,从绿地、园林地、耕地以及荒废地4种不同土地利用类型土壤进行采样研究。研究结果表明:4种不同土地利用类型土壤中主要菌种为细菌、真菌以及放线菌,放线菌比例最大,其次是细菌,真菌比例最小。采样深度、温度、土地利用类型及含水率均影响微生物群落特征。随着采样深度的增加,4种土地利用类型土壤中微生物数量不断减少,0～10cm微生物总数最多。荒废地土壤微生物数量最多,因为荒废地土层中有机质含量高,为微生物的生长提供了营养物质。含水率过高或过低均不利于微生物生长,当处于最佳含水率时微生物数量最大。对于绿地和园林地而言,最佳含水率为10%～15%,耕地最佳含水率为15%～20%,荒废地最佳含水率为10%左右。     

Al3+胁迫对茶园土壤微生物区系及生理群的影响

以茶园土壤为研究对象,通过外源添加Al3+溶液,研究了Al3+胁迫对茶园土壤微生物区系及生理群的影响.结果表明,茶园土壤中的不同种类的微生物对Al3+的敏感性不同,Al3+添加量升至0.8 g/kg时,放线菌、真菌有一定的耐受性,而细菌数量呈快速下降趋势,亚硝化细菌几乎不能成活,但随着Al3+添加量的进一步升高,放线菌...     

抗生素菌渣堆肥进程中微生物群落的变化

将青霉素菌渣、林可霉素菌渣与牛粪等原料分别进行好氧堆肥实验，以考察堆肥过程中不同菌渣对微生物群落的影响。在堆制的41d里，根据温度变化分阶段采集堆肥样品，采用稀释倒平板法测定细菌、放线菌和真菌的数量。结果表明，菌渣不同，其堆肥中的微生物群落变化趋势不同。青霉素菌渣堆肥中细菌数量变化趋势为高一低，真菌数量变化趋势为高一低．高，放线菌数量为逐渐增加；林可霉素菌渣堆肥过程中细菌数量变化趋势为低一高一低，放线菌和真菌数量变化趋势为高．低．高。依据真菌菌落形态观察，菌渣堆肥中的真菌种类比对照牛粪堆肥单一，表明两种菌渣对堆肥中的微生物多样性均产生了不利影响。林可霉素菌渣堆肥初始时的细菌数量比对照低1个数量级，放线菌数量在整个堆肥进程中都明显低于对照，堆肥结束时，随着菌渣含量的增加，放线菌数量逐渐下降，高温期真菌数量下降幅度随着菌渣含量增加而加大，表明林可霉素菌渣对细菌、放线菌和真菌均有不同程度的抑制。堆肥化后菌渣中林可霉素残留量的减少表明，在一定条件下堆肥处理可以将抗生素菌渣无害化和资源化。     

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。     

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％.     

PLA对土壤微生物生长的影响及PLA的生物降解性

从不同土壤环境中筛选出的4类不同土壤微生物91株,分别标记为细菌、固氮菌、分解纤维素菌和放线菌。然后通过将定量的聚乳酸（PLA）分别加入对应液态培养基中,恒温（30℃）摇床培养,连续测定这4类不同的土壤微生物对PLA的降解性能以及该种聚合物对各种微生物生长的影响。结果表明,虽然在自然界中PLA的降解率比较高,但不同类型的土壤微生物对PLA的降解性能却存在明显个体差异。在测试期内,放线菌对于PLA的总降解率最高;而细菌中RB-4的日降解率最高,达到3%左右;纤维分解菌HX-8及固氮菌RG-28的日降解率能达到2.4%。PLA降解产物对于细菌及纤维分解菌的抑制性普遍较强。     

陕北石油污染区土壤细菌群落结构解析

为了解陕北地区石油污染对土壤微生物群落结构的影响,采用高通量测序对石油污染土壤中细菌群落结构进行研究,考察了石油污染土样的理化性质、可培养微生物数量及细菌群落结构,探讨石油污染程度与细菌群落结构间的关系。结果表明,石油污染土样中残油量为28.7~870.0mg/kg,相对于未污染土样,石油污染土样的总碳随残油量的增加呈增加趋势。石油污染土样中可培养细菌数量大于未污染土样,而可培养放线菌数量则相反。细菌群落结构分析表明,石油污染土样中细菌群落数量显著低于未污染土样,操作分类单元(OTU)数从未污染土样的7 707个最低下降到2 034个,且物种丰富度显著降低,其中厚壁菌门、放线菌门及变形菌门为优势菌群,随土壤残油量增加,厚壁菌门、变形菌门及拟杆菌门比例显著上升,而酸杆菌门、芽单胞菌门等比例则显著降低。     

造纸废水灌溉对黄河三角洲退化湿地可培养土壤微生物的影响

利用造纸废水恢复重度退化湿地，分析了土壤微生物数量、土壤呼吸强度及微生物量碳的变化情况。结果表明，灌溉后，8月份，细菌和真菌数量最多，放线菌5月份数量最多；细菌、真菌、放线菌各灌水深度上层大于中层，各灌水深度、细菌、真菌、放线菌上层数量均大于对照；土壤呼吸主要发生在表层（0~20 cm）；8月份，微生物量碳达到最大值690.3 mg/kg，且上中下层依次递减。相关分析表明，15 cm灌水量，土壤呼吸强度与有机碳呈极显著正相关（r=0.996，P=0.0036），灌水量为0、5、10和20 cm，土壤微生物量碳与有机碳呈极显著正相关(r=0.999，0.999，0.999；P<0.001)，15 cm灌水量，微生物量碳与速效磷呈极显著正相关（r=0.972，P=0.028）；5 cm灌水量，微生物总数与有机碳呈显著线性正相关（r=0.953，P=0.047），对照和15 cm灌水量，微生物总数与速效磷呈显著正相关（r=0.976，P=0.024；r=0.968；P=0.032）。灌溉处理后的造纸废水，可增加重度退化湿地土壤微生物的活性，改善土壤质量。     

固定化耐低温混合菌对焦化土壤多环芳烃的降解研究

研究了固定化耐低温真菌-细菌混合菌在低温环境下,对焦化厂污染土壤中的菲(Phe)和苯并[b]荧蒽(BbF)降解的动态变化,利用高通量测序技术分析了降解过程中微生物群落多样性变化。结果表明:在低温条件下固定化混合菌对土壤中Phe、BbF的去除率远高于游离混合菌与固定化单菌,在60d的降解周期下,固定化混合菌对土壤中Phe和BbF的降解率分别可达59.61%和45.24%。处理前,土壤中细菌与真菌初始Shannon多样性指数分别为2.79和0.33,细菌远高于真菌,土壤中土著微生物以细菌为主,高丰度的细菌抑制了真菌的生长代谢。处理后,细菌的Shannon多样性指数下降至1.33,真菌的Shannon多样性指数增加至1.01,Phe和BbF的降解与细菌多样性呈负相关,且细菌多样性的降低减少了其对真菌的抑制作用。对比分析了处理前后土壤中微生物群落组成的变化,结果表明:投加固定化混合菌后,固定化混合菌中的假单胞菌(Pseudomonas sp.)SDR4和高山被孢霉(Mortierella alpina)JDR7在低温下生长代谢良好,并成为降解过程中的优势菌,其物种相对丰度分别提高至79.84%与58.63%。固定化混合菌对低温环境有良好的耐性,固定化混合菌的投加提高了菌株对多环芳烃(PAHs)的生物利用有效性,改变了土壤中微生物群落的结构和丰度,可应用于低温土壤PAHs的原位修复。     

Alterations of microbial populations and composition in the rhizosphere and bulk soil as affected by residual acetochlor

Acetochlor is a widely used herbicide in maize fields; however, the ecological risk of its residue in the soil–plant system remains unknown. We investigated the dissipation dynamics of field dose acetochlor and clarified its impact on microbial biomass and community structure both in the rhizosphere and bulk soil over 1 month after its application. Soil microbial parameters such as quantities of culturable bacteria and fungi represented by colony-forming units, soil microbial biomass carbon (SMB_C), and phospholipid fatty acids (PLFAs) were determined across different sampling times. The results showed that the dissipation half-lives of acetochlor were, respectively, 2.8 and 3.4 days in the rhizosphere and bulk soil, and 0.02–0.07 μg/g residual acetochlor could be detected in the soil 40 days after its application. Compared to the bulk soil, microbial communities in the rhizosphere soil were inclined to be affected by the application of acetochlor: SMB_C content and bacterial growth were most likely to be increased; however, fungal growth was prone to be inhibited. The principal component analysis of PLFAs, as well as the comparisons of fungi/bacteria and cy17:0/C16:1ω9c ratios between different treatments over sampling time, revealed that the soil microbial community composition was significantly affected by acetochlor at its early application stage (at day 15); thereafter, the effects of acetochlor were attenuated or even could not be detected. Our results suggested that residual acetochlor did not confer a long-term impairment on viable bacterial groups in the rhizosphere and bulk soil.     

The fate of herbicide acetochlor and its toxicity to Eisenia fetida under laboratory conditions

To assess the toxic effects of the herbicide acetochlor on earthworms, we exposed Eisenia fetida (Savigny) to artificial soils (OECD soil) supplemented with different concentrations (5, 10, 20, 40 and 80 mg kg-1 soil) of acetochlor. The residues of acetochlor in soil and the effect of the herbicide on growth, reproduction, glutathione-S-transferases (GST) activity and cellulase activity of earthworms were determined. The degradation half-life of acetochlor in soil of acetochlor was between 9.3 and 15.6 days under laboratory condition; the degradation rate with low concentrations was faster than it was with higher concentrations. At 5 and 10 mg kg-1, acetochlor had not significant effect on growth of E. fetida except after 15 and 30 days of exposure. When concentration>20 mg kg-1, growth rates and numbers of juveniles per cocoon decreased significantly compared to the control in all treatments. However, cellulase activity decreased significantly in all treatments (5-80 mg kg-1). This study showed that acetochlor had no long-term effect on the growth and reproduction of E. fetida at field dose (5-10 mg kg-1). At higher concentrations of acetochlor (20-80 mg kg-1), acetochlor revealed sublethal toxicity to E. fetida. Growth, numbers of juveniles per cocoon and cellulase activity can be regarded as sensitive parameters to evaluate the toxicity of acetochlor on earthworms.     

Degradation and detoxification of acetochlor in soils treated by organic and thiosulfate amendments

This work investigated the degradation and detoxification of acetochlor in a soil amended with an organic fertilizer or sodium thiosulfate (STS). Over an incubation period of 28 d, the residual acetochlor was measured, soil dehydrogenase activity was determined, and major degradates were identified. Results show that high-concentration acetochlor was persistent in the soil, as indicated by the depression in soil dehydrogenase activity. When the soil was amended with the organic fertilizer, the soil dehydrogenase activity was stimulated by supplemented nutrients, which resulted in a higher degradation of acetochlor. While STS did not significantly stimulate the soil dehydrogenase activity, acetochlor degraded more rapidly in STS-amended soil than in organic-amended soil. The Wright-Hobbie plots show that the influence of initial acetochlor concentration on degradation was dependent on the amendments. While the organic amendment resulted in the same degradate of acetochlor ethanesulfonic acid as in unamended soil, the STS amendment produced dechlorinated acetochlor thiosulfonic acid. The degradation of acetochlor in organic- and STS-amended soils thus occurred via different mechanisms. Further tests show that both degradates were less toxic to green algae than acetochlor. Both organic and STS amendments thus effectively degrade and detoxify acetochlor in soils.     

Effect of soil and sediment composition on acetochlor sorption and desorption

Background, aim, and scope  Herbicide fate and its transport in soils and sediments greatly depend upon sorption–desorption processes. Quantitative determination of herbicide sorption–desorption is therefore essential for both the understanding of transport and the sorption equilibrium in the soil/sediment–water system; and it is also an important parameter for predicting herbicide fate using mathematical simulation models. The total soil/sediment organic carbon content and its qualitative characteristics are the most important factors affecting sorption–desorption of herbicides in soil or sediment. Since the acetochlor is one of the most frequently used herbicides in Slovakia to control annual grasses and certain annual broad-leaved weeds in maize and potatoes, and posses various negative health effects on human beings, our aim in this study was to investigate acetochlor sorption and desorption in various soil/sediment samples from Slovakia. The main soil/sediment characteristics governing acetochlor sorption–desorption were also identified. Materials and methods  The sorption–desorption of acetochlor, using the batch equilibration method, was studied on eight surface soils, one subsurface soil and five sediments collected from the Laborec River and three water reservoirs. Soils and sediments were characterized by commonly used methods for their total organic carbon content, distribution of humus components, pH, grain-size distribution, and smectite content, and for calcium carbonate content. The effect of soil/sediment characteristics on acetochlor sorption–desorption was examined by simple correlation analysis. Results  Sorption of acetochlor was expressed as the distribution coefficient (K _d). K _d values slightly decreased as the initial acetochlor concentration increased. These values indicated that acetochlor was moderately sorbed by soils and sediments. Highly significant correlations between the K _d values and the organic carbon content were observed at both initial concentrations. However, sorption of acetochlor was most closely correlated to the humic acid carbon, and less to the fulvic acid carbon. The total organic carbon content was found to also significantly influence acetochlor desorption. Discussion  Since the strong linear relationship between the K _d values of acetochlor and the organic carbon content was already released, the corresponding K _oc values were calculated. Considerable variation in the K _oc values suggested that other soil/sediment parameters besides the total soil organic carbon content could be involved in acetochlor sorption. This was revealed by a significant correlation between the K _oc values and the ratio of humic acid carbon to fulvic acid carbon (C_HA/C_FA). Conclusions  When comparing acetochlor sorption in a range of soils and sediments, different K _d values which are strongly correlated to the total organic carbon content were found. Concerning the humus fractions, the humic acid carbon content was strongly correlated to the K _d values, and it is therefore a better predictor of the acetochlor sorption than the total organic carbon content. Variation in the K _oc values was attributed to the differences in distribution of humus components between soils and sediments. Desorption of acetochlor was significantly influenced by total organic carbon content, with a greater organic carbon content reducing desorption. Recommendations and perspectives  This study examined the sorption–desorption processes of acetochlor in soils and sediments. The obtained sorption data are important for qualitative assessment of acetochlor mobility in natural solids, but further studies must be carried out to understand its environmental fate and transport more thoroughly. Although, the total organic carbon content, the humus fractions of the organic matter and the C_HA/C_FA ratio were sufficient predictors of the acetochlor sorption–desorption. Further investigations of the structural and chemical characteristics of humic substances derived from different origins are necessary to more preciously explain differences in acetochlor sorption in the soils and sediments observed in this study.     

Combined bioremediation of atrazine-contaminated soil by <Emphasis Type="Italic">Pennisetum</Emphasis> and <Emphasis Type="Italic">Arthrobacter</Emphasis> sp. strain DNS10

Strain DNS10 was isolated from the black soil collected from the northeast of China which had been cultivated with atrazine as the sole nitrogen source. Pennisetum is a common plant in Heilongjiang Province of China. The main objective of this paper was to evaluate the efficiency of plant–microbe joint interactions (Arthrobacter sp. DNS10 + Pennisetum) in atrazine degradation compared with single-strain and single-plant effects. Plant–microbe joint interactions degraded 98.10 % of the atrazine, while single strain and single plant only degraded 87.38 and 66.71 % after a 30-day experimental period, respectively. The results indicated that plant–microbe joint interactions had a better degradation effect. Meanwhile, we found that plant–microbe joint interactions showed a higher microbial diversity. The results of microbial diversity illustrated that the positive effects of cropping could improve soil microbial growth and activity. In addition, we planted atrazine-sensitive plants (soybean) in the soil after repair. The results showed that soybean growth in soil previously treated with the plant–microbe joint interactions treatment was better compared with other treatments after 20 days of growth. This was further proved that the soil is more conducive for crop cultivation. Hence, plant–microbe joint interactions are considered to be a potential tool in the remediation of atrazine-contaminated soil.     

Effects of metsulfuron-methyl on the microbial population and enzyme activities in wheat rhizosphere soil

The effects of metsulfuron-methyl, a sulfonylurea herbicide, on the wheat soil microorganisms were evaluated by the methods of microbial inoculation culture, and the activities of three enzymes were measured using the colorimetric method. The tolerant microorganisms that can resist 500 microg x g(-1) metsulfuron-methyl in the counting culture medium were studied specially. Metsulfuron-methyl distinctly inhibited the common aerobic heterotriphic bacteria, but the effects on common fungi and common actinomycete were not evident. In the meantime, the number of tolerant fungi increased greatly in the rhizosphere after the application of metsulfuron-methyl in contrast to the significant decrease of the amount of tolerant actinomycete. It indicates that fungi might turn into the dominant microbial type and actinomycete is the sensitive factor in the soil polluted by sulfonylurea residues. The population of aromatic compounds-decomposing bacteria, aerobic azotobacter, and nitrite bacteria all increased in the earlier period, but the aerobic azotobacter decreased rapidly in number 30 days later, and the amount of nitrite bacteria also showed a temporary decrease with time 15 days later. However, the denitrifying bacteria just began to increase significantly after the crops had grown for 50 days. The amount of sulfur-oxidizing bacteria gradually decreased with the growth of crops, and so were the sulfate-reducing bacteria after metsulfuron-methyl application. To all types of microorganisms, there were more microbes in rhizosphere samples than those in nonrhizosphere except aerobic azotobacter. It means the growth of wheat root system can stimulate the growth of most microorganisms. The activities of hydrogen peroxidase and polyphenol oxidase in soil samples after metsulfuron-methyl application were notably lower than those in the control, and the difference of the activities between the samples of rhizosphere and nonrhizosphere was evident. On the contrary, the activity of dehydrogenase was not inhibited by the application of metsulfuron-methyl, and the rhizosphere effect was not obvious either.     

Biomarkers responses of the earthworm Eisenia fetida to acetochlor exposure in OECD soil

To examine the potential of a suite of biomarkers as early warning indicators of environmental pollution, sperm count, neutral red retention time (NRRT) and DNA damage were measured in earthworm Eisenia fetida exposed to increasing concentrations of acetochlor in OECD soil. The neutral red retention time of earthworms coelomocytes was sensitive to acetochlor pollution, and decreased significantly when the concentration was more than 10mgkg(-1) after 30 and 60 days of exposure (P<0.05). The reduced neutral red retention time correlated with the soil acetochlor residual. Sperm count decreased significantly at the concentrations of 40 and 80mgkg(-1) after 15 days of exposure (P<0.05). The DNA damage of earthworms coelomocytes increased significantly after 30 days of exposure at the highest concentration (80mgkg(-1); P<0.05). Earthworms were under physiological stress at field dose of acetochlor (10mgkg(-1)). Higher concentrations of acetochlor caused sperm count decrease and DNA damage of earthworms. Such a suite of biomarkers could serve as indicators of the health of the soil environment and to evaluate the toxicity of acetochlor on earthworms or as a means of monitoring soil acetochlor pollution.     

Effects of Metsulfuron-Methyl on the Microbial Population and Enzyme Activities in Wheat Rhizosphere Soil

The effects of metsulfuron-methyl, a sulfonylurea herbicide, on the wheat soil microorganisms were evaluated by the methods of microbial inoculation culture, and the activities of three enzymes were measured using the colorimetric method. The tolerant microorganisms that can resist 500 μ g·g^?1 metsulfuron-methyl in the counting culture medium were studied specially. Metsulfuron-methyl distinctly inhibited the common aerobic heterotriphic bacteria, but the effects on common fungi and common actinomycete were not evident. In the meantime, the number of tolerant fungi increased greatly in the rhizosphere after the application of metsulfuron-methyl in contrast to the significant decrease of the amount of tolerant actinomycete. It indicates that fungi might turn into the dominant microbial type and actinomycete is the sensitive factor in the soil polluted by sulfonylurea residues. The population of aromatic compounds–decomposing bacteria, aerobic azotobacter, and nitrite bacteria all increased in the earlier period, but the aerobic azotobacter decreased rapidly in number 30 days later, and the amount of nitrite bacteria also showed a temporary decrease with time 15 days later. However, the denitrifying bacteria just began to increase significantly after the crops had grown for 50 days. The amount of sulfur-oxidizing bacteria gradually decreased with the growth of crops, and so were the sulfate-reducing bacteria after metsulfuron-methyl application. To all types of microorganisms, there were more microbes in rhizosphere samples than those in nonrhizosphere except aerobic azotobacter. It means the growth of wheat root system can stimulate the growth of most microorganisms. The activities of hydrogen peroxidase and polyphenol oxidase in soil samples after metsulfuron-methyl application were notably lower than those in the control, and the difference of the activities between the samples of rhizosphere and nonrhizosphere was evident. On the contrary, the activity of dehydrogenase was not inhibited by the application of metsulfuron-methyl, and the rhizosphere effect was not obvious either.     

Influence of root-exudates concentration on pyrene degradation and soil microbial characteristics in pyrene contaminated soil

The effect of ryegrass (Lolium perenne L.) root-exudates concentration on pyrene degradation and the microbial ecological characteristics in the pyrene contaminated soil was investigated by simulating a gradually reducing concentration of root exudates with the distance away from root surface in the rhizosphere. Results showed that, after the root-exudates were added 15 d, the pyrene residue in contaminated soil responded nonlinearly in the soils with the same pyrene contaminated level as the added root-exudates concentration increased, which decreased first and increased latter with the increase of the added root-exudates concentration. The lowest pyrene concentration appeared when the root exudates concentration of 32.75 mg kg(-1) total organic carbon (TOC) was added. At the same time, changes of microbial biomass carbon (MBC, C(mic)) and microbial quotient (C(mic)/C(org)) were opposite to the trend of pyrene degradation as the added root-exudates concentration increased. Phospholipid fatty acid (PLFA) analysis revealed that bacteria was the dominating microbial community in pyrene contaminated soil, and the changing trends of pyrene degradation and bacteria number were the same. The changing trend of endoenzyme-dehydrogenase activity was in accordance with that of soil microbe, indicating which could reflect the quantitative characteristic of detoxification to pyrene by soil microbe. The changes in the soils microbial community and corresponding microbial biochemistry characteristics were the ecological mechanism influencing pyrene degradation with increasing concentration of the added root-exudates in the pyrene contaminated soil.     

含莠去津和乙草胺河水灌溉对苗期水稻危害的研究

本文以１９８８、１９９２和１９９３年洋河流域张家口市部分水稻田污染受害事故为背景，通过事故现场调查资料分析、洋河水质监测、宣化区污染源调查、水稻的药害暴露实验和模型计算，研究了含有除草剂莠去津和乙草胺的河水灌溉对苗期水稻的危害。结果显示，河水中莠去津和乙草胺对水稻苗期的安全灌溉浓度分别为０．０１ｍｇ／Ｌ和０．０５ｍｇ／Ｌ；河水中莠去津对水稻的致死浓度是０．１ｍｇ／Ｌ；ｐＨ、ＮＨ３－Ｎ和表面活性剂对这种危害作用具有一定的协同效应；为了满足河水对水稻的灌溉水质要求，污染源允许排放的莠去津和乙草胺分别为１．０ｋｇ／ｄ和２．０ｋｇ／ｄ。