铜污染土壤微生物群落结构及酶活性研究

The microbial community structure and enzyme activities of seven paddy soils with different Cu concentrations were investigated in the vicinity of a Cu smelter in Fuyang County,Zhejiang Province in Southeast China.The microbial community structure was analyzed using the phospholipid fatty acid (PLFA) and multiplex-terminal restriction fragment length polymorphism (M-TRFLP) techniques.There was no clear dose-response relationship between Cu pollution and soil enzyme activity except for urease.Both PLFA and M-TRFLP methods showed that Cu contamination had a large effect on the soil microbial community structure.PLFA indicators of Gram-positive bacteria (16:0i,15:0i) and fungi (18:2w6,9) relatively decreased with increasing Cu concentration,whereas indicators of Gram-negative bacteria (19:0cy,16:1w7) increased.The M-TRFLP results suggested that there was a dose-dependent response between Cu pollution and bacterial community or fungal community.The fungal community was more sensitive to Cu pollution than the bacterial community.There were no significant differences in archaeal community structure between the different Cu pollution plots and archaea might be more tolerant to Cu pollution than both bacteria and fungi.     

干旱热带地区土地利用变化对土壤微生物群落组成及有机碳含量的影响

Restoration of forests poses a major challenge globally,particularly in the tropics,as the forests in these regions are more vulnerable to land-use change.We studied land-use change from natural forest (NF) to degraded forest (DF),and subsequently to either Jatropha curcas plantation (JP) or agroecosystem (AG),in the dry tropics of Uttar Pradesh,India,with respect to its impacts on soil microbial community composition as indicated by phospholipid fatty acid (PLFA) biomarkers and soil organic carbon (SOC) content.The trend of bacterial PLFAs across all land-use types was in the order:NF ＞ JP ＞ DF＞ AG.In NF,there was dominance of gram-negative bacterial (G-) PLFAs over the corresponding gram-positive bacterial (G+) PLFAs.The levels of G-PLFAs in AG and JP differed significantly from those in DF,whereas those of G+ PLFAs were relatively similar in these three land-use types.Fungal PLFAs,however,followed a different trend:NF ＞ JP ＞ DF =AG.Total PLFAs,fungal/bacterial (F/B) PLFA ratio,and SOC content followed trends similar to that of bacterial PLFAs.Across all land-use types,there were strong positive relationships between SOC content and G-,bacterial,fungal,and total microbial PLFAs and F/B PLFA ratio.Compared with bacterial PLFAs,fungal PLFAs appeared to be more responsive to land-use change.The F/B PLFA ratio,fungal PLFAs,and bacterial PLFAs explained 91％,94％,and 73％ of the variability in SOC content,respectively.The higher F/B PLFA ratio in JP favored more soil C storage,leading to faster ecosystem recovery compared to either AG or DF.The F/B PLFA ratio could be used as an early indicator of ecosystem recovery in response to disturbance,particularly in relation to land-use change.     

北美中部大平原半干旱农业生态系统中覆盖作物和灌溉对土壤微生物群落和酶活性的影响

Cover crops can have beneficial effects on soil microbiology by increasing carbon (C) supply, but these beneficial effects can be modulated by precipitation conditions. The objective of this study was to compare a fallow-winter wheat (Triticum aestivum L.) rotation to several cover crop-winter wheat rotations under rainfed and irrigated conditions in the semiarid US High Plains. Experiments were carried out at two sites, Sidney in Nebraska and Akron in Colorado, USA, with three times of soil sampling in 2012--2013 at cover crop termination, wheat planting, and wheat maturity. The experiments included four single-species cover crops, a 10-species mixture, and a fallow treatment. The variables measured were soil C and nitrogen (N), soil community structure by fatty acid methyl ester (FAME) profiles, and soil β-glucosidase, β-glucosaminidase, and phosphodiesterase activities. The fallow treatment, devoid of living plants, reduced the concentrations of most FAMEs at cover crop termination. The total FAME concentration was correlated with cover crop biomass (R = 0.62 at Sidney and 0.44 at Akron). By the time of wheat planting, there was a beneficial effect of irrigation, which caused an increase in mycorrhizal and protozoan markers. At wheat maturity, the cover crop and irrigation effects on soil FAMEs had subsided, but irrigation had a positive effect on the β-glucosidase and phosphodiesterase activities at Akron, which was the drier of the two sites. Cover crops and irrigation were slow to impact soil C concentration. Our results show that cover crops had a short-lived effect on soil microbial communities in semiarid wheat-based rotations and irrigation could enhance soil enzyme activity. In the semiarid environment, longer time spans may have been needed to see beneficial effects of cover crops on soil microbial community structure, soil enzyme activities, and soil C sequestration.     

土壤微食物网对旱改水不同稻作年限土地利用变化的响应

Land use changes affect belowground ecosystems.During the past few decades,land use in Northeast China has changed considerably,and the area of paddy fields has increased rapidly from upland.In this study,soil characteristics and soil biotic community in paddy fields with different years of rice cultivation were measured to examine the effects of land use change from upland to paddy fields on soil micro-food web.The upland maize fields were selected as control and the microbial community composition was characterized using phospholipid fatty acids (PLFAs) analysis.The microbial biomass (total PLFA),bacteria biomass,and fungi biomass were higher in the 20-40-year (late-stage) than 1-10-year (early-stage) paddy fields.The abundances of total nematodes and bacterivores were lower in the early-stage than late-stage paddy fields.The abundance of herbivores was the highest in the early-stage paddy fields but that of omnivore-predators was the highest in the late-stage paddy fields.Structural equation model indicated that soil food web was developed and structured after 20 years of paddy cultivation.Our results suggested that soil micro-food web may be a good indicator for soil development and stabilization of paddy fields following land use change.     

蚯蚓与黑麦草相互作用对土壤中荧蒽去除的影响

Earthworms can promote the bioremediation of contaminated soils through enhancing plant growth and microorganism development. The individual and combined effects of earthworms and ryegrass (Lolium multiflorum Lam.) on the removal of fluoranthene from a sandy-loam alluvial soil were investigated in a 70-d microcosm experiment. The experiment was set up in a complete factorial design with treatments in four replicates: without earthworms or ryegrass (control, CK), with earthworms only (E), with ryegrass only (P), and with both earthworms and ryegrass (EP). The residual fluoranthene, microbial biomass C, and polyphenol oxidase activity in the soil changed significantly (P<0.01) with time. In general, the residual concentration of fluoranthene in the soil decreased sharply from 71.8-88.7 to 31.7-37.4 mg kg 1 in 14 d, and then decreased gradually to 19.7-30.5 mg kg 1 on the 70th d. The fluoranthene concentration left in the soil was the least with both earthworms and ryegrass, compared to the other treatments at the end of the experiment. Half-life times of fluoranthene in the E, P, and EP treatments were 17.8%-36.3% smaller than that of CK. More fluoranthene was absorbed by earthworms than ryegrass. However, the total amounts of fluoranthene accumulated in both the ryegrass and earthworms were small, only accounting for 0.01%-1.20% of the lost fluoranthene. Therefore, we assumed that microbial degradation would play a dominant functional role in fluoranthene removal from soil. We found that earthworms significantly increased microbial biomass C and polyphenol oxidase activity (P<0.01) in the presence of ryegrass at the end of the experiment. Furthermore, microbial biomass C and polyphenol oxidase activity were significantly (P<0.05) and negatively related to the residual fluoranthene concentration. This implied that earthworms might promote the removal of fluoranthene from soil via stimulating microbial biomass C and polyphenol oxidase activity.     

重复添加植物残体后土壤微生物活性和生物量对盐度的响应特征

Microbial adaptation to salinity can be achieved through synthesis of organic osmolytes,which requires high amounts of energy;however,a single addition of plant residues can only temporarily improve energy supply to soil microbes.Therefore,a laboratory incubation experiment was conducted to evaluate the responses of soil microbes to increasing salinity with repeated additions of plant residues using a loamy sand soil with an electrical conductivity in saturated paste extract（EC_e） of 0.6 dS m^-1.The soil was kept non-saline or salinized by adding different amounts of NaCl to achieve EC_e of 12.5,25.0 and 50.0 dS m^-1.The non-saline soil and the saline soils were amended with finely ground pea residues at two rates equivalent to 3.9 and 7.8 g C kg^-1 soil on days 0,15 and29.The soils receiving no residues were included as a control.Cumulative respiration per g C added over 2 weeks after each residue addition was always greater at 3.9 than 7.8 g C kg^-1 soil and higher in the non-saline soil than in the saline soils.In the saline soils,the cumulative respiration per g C added was higher after the second and third additions than after the first addition except with3.9 g C kg^-1 at EC_e of 50 dS m^₁.Though with the same amount of C added(7.8 g C kg^-1),salinity reduced soil respiration to a lesser extent when 3.9 g C kg^-1 was added twice compared to a single addition of 7.8 g C kg^-1.After the third residue addition,the microbial biomass C concentration was significantly lower in the soils with EC_e of 25 and 50 dS m^₁ than in the non-saline soil at3.9 g C kg^-1,but only in the soil with EC_e of 50 dS m^-1 at 7.8 g C kg^-1.We concluded that repeated residue additions increased the adaptation of soil microbial community to salinity,which was likely due to high C availability providing microbes with the energy needed for synthesis of organic osmolytes.     

利用复合方法对不同耕作系统中的土壤微生物活性进行分析

Cropping activities may affect soil microbial activities and biomass,which would affect C and N cycling in soil and thus the crop yields and quality.In the present study,a combination of microcalorimetric,enzyme activity(sucrase,urease,catalase,and fluorescein diacetate hydrolysis),and real-time polymerase chain reaction(RT-PCR) analyses was used to investigate microbial status of farmland soils,collected from 5 different sites in Huazhong Agriculture University,China.Our results showed that among the 5sites,both positive and negative impacts of cropping activities on soil microbial activity were observed.Enzyme activity analysis showed that cropping activities reduced soil sucrase and urease activities,which would influence the C and N cycles in soil.Much more attentions should be given to microbial status affected by cropping activities in future.According to the correlation analysis,fluorescein diacetate hydrolysis showed a significantly(P 0.05) negative correlation with the time to reach the maximum power output(R ——0.898),but a significantly(P 0.05) positive correlation with bacterial gene copy number(R = 0.817).Soil catalase activity also showed a significantly(P 0.05) positive correlation with bacterial gene copy number(R = 0.965).Using combined methods would provide virtual information of soil microbial status.     

中国土壤微生物量的大小

The microbial biomass C, N and P of soils all over China were determined in this study to study their affecting factors. The results, about 100-417 mg C kg^-1 soil, 18-51 mg N kg^-1 soil and 4.4-27.3 mg P kg^-1 soil, showed the biomass C, N and P in linear relationship with the soil total organic C, toal N and soil organic P. The ratios of C: N and C:P, ranging from 5.6 to 9.6 and from 11.2 to 48.4 respectively, were affected by soil pH, texture, crop rotation, macroclimate, etc. The ratio of C:N in soil biomass increases gradually from the north to the south in China.     

黄土高原中国松人工林演替过程中的土壤微生物和酶活性

Successional and seasonal effects on soil microbial and enzymatic properties were studied in Chinese pine (Pinus tabu- laeformis) plantations in an age sequence of 3-, 7-, 13-, 21- and 28-year-old in northern Ziwuling region in the middle of Loess Plateau, China. The results indicated that plantation age and season affected soil microbial and enzymatic parameters significantly. Soil organic C, total N, microbial biomass C, microbial quotient, basal respiration, dehydrogenase, N-α-benzoyl-L-argininamide (BAA)-protease, urease and β-glucosidase increased quickly and tended to be highest at PF21 (21-year plantation), thereafter they remained nearly at a constant level, whereas the metabolic quotient (qCO 2 ) showed an initial increase and then decreased gradually. Measures of these soil properties showed significant seasonal fluctuations except for organic C and total N, which were found to be relatively stable throughout the study period, and the seasonal distributions were autumn spring summer winter for microbial biomass C, microbial quotient, dehydrogenase, and β-glucosidase; autumn summer spring winter for BAA-protease and urease; and summer autumn spring winter for basal respiration and qCO 2 . Significant season × age interaction was observed for biomass C, basal respiration, dehydrogenase and BAA-protease.     

黄土高原某些耕作土壤中土壤微生物生物量C、N与矿化N的关系

The chloroform fumigation-incubation method was used to measure the soil microbial biomass C (SMBC) and N (SMBN) in 16 loessial soils sampled from Ansai, Yongshou and Yangling in Shaanxi Province. The SMBC contents in the soils ranged from 75.9 to 301.0 μg C g^-1 with an average of 206.1 μg C g^-1, accounting for 1.36%~6.24% of the total soil organic C with an average of 3.07%, and the SMBN contents from 0.51 to 68.40 μg N g^-1 with an average of 29.4 μg N g^-1, accounting for 0.20%~5.65% of the total N in the soils with an average of 3.36%. A close relationship was found between SMBC and SMBN, and they both were positively correlated with total organic C, total N, NaOH hydrolizable N and mineralizable N. These results confirmed that soil microbial biomass had a comparative role in nutrient cycles of soils.     

土壤微生物群落对高剂量的新鲜橄榄油厂废水的响应

An incubation experiment was designed in order to determine the further microbiological response to an addition (500 m³ ha^-1) of fresh olive mill wastewater (FOMWW) in a soil that has been frequently amended with uncontrolled doses of OMWW since 90s in an active disposal site (ADS soil). To achieve this aim, the phospholipid fatty acid (PLFA) profiles, microbial biomass C (C_mic), and dehydrogenase (DHA) and urease activities (URA) were monitored at the beginning (T₀), 3 h (T₁) and 97 d (T_f, i.e., the end) of incubation after FOMWW addition. After the FOMWW addition, an increase in the ratio of fungal to bacterial PLFAs was observed in ADS soil. Moreover, a relative increase of monounsaturated fatty acids (MUFAs) with respect to saturated fatty acids (SATFA) was found in the ADS soil. An increase of the Gram-positive to Gram-negative ratio was observed in this soil at the end of the incubation. While DHA and Cmic increased in the ADS soil after FOMWW addition, URA showed a decrease. Fungi and Gram-positive bacterial biomass experienced an increase after addition of a high dose of FOMWW in laboratory conditions.     

Soil microbial communities changed with a continuously monocropped processing tomato system

To reveal the regulatory mechanisms underlying the productivity of long-term continuous cropping of processing tomato, a multi-year study was carried out to understand the effects of long-term continuous cropping on the community structures of the root zone microbes. Soil samples collected from continuous cropping of processing tomato after 3, 5 and 7 years were used for this study. Results showed that soil microbial biomass C (SMBC), N (SMBN) and microbial quotient (qMB) significantly decreased with longer cropping. After seven years of continuous cropping, the SMBC and SMBN contents, and qMB respectively significantly decreased by 52.3%, 78.8% and 48.2% (p?相似文献   

改变凋落物和根系输入对米槠天然林土壤微生物群落的影响

伴随气候变化下亚热带地区米槠天然林净初级生产力变化,凋落物以及植物根系输入亦会发生改变,这将显著影响土壤微生物群落。于2019年7月在设置7年的米槠天然林植物残体添加和去除试验（the detritus input and removal treatments,DIRT）样地采集不同处理（对照、去除地上凋落物、去除地下根系、无凋落物输入、添加双倍地上凋落物）的2个土层土壤（0—10,10—20 cm）,测定微生物磷脂脂肪酸（phospholipid fatty acid,PLFA）含量,计算各微生物群落比值以及多样性,进一步揭示凋落物和植物根系输入对亚热带米槠天然林土壤微生物群落组成和多样性的影响。结果表明：（1）不同处理下0—10 cm土层微生物磷脂脂肪酸含量约为10—20 cm土层的2倍;（2）地上凋落物变化均使得革兰氏阳性菌、阴性菌及放线菌等细菌含量出现不同程度的下降,但不会对丛枝菌根等真菌含量产生影响,而去除根系处理显著降低丛枝菌根真菌含量;（3）微生物群落Shannon-wiener、Simpson多样性指数不受凋落物输入的影响,凋落物去除降低表层土壤微生物群落的Margalef丰富度,提高Pielou均匀度,表明0—10 cm土层微生物群落含量与分布状况受凋落物输入变化影响较大;（4）地下植物根系存在可提高真菌（如丛枝菌根真菌）含量,而地上凋落物输入主要改变细菌丰度以及群落结构。可溶性有机碳以及矿质氮是影响不同处理土壤微生物群落组成和多样性的主要因素。可见,凋落物和根系输入通过土壤理化性质的变化而影响了微生物群落,研究结果可为全面认识植物、土壤与微生物间的相互作用对森林生产力的影响提供科学依据。     

浇灌木醋液和添加粉煤灰对煤矸石基质微生物群落的影响

大量煤矸石的堆放严重影响了矿区的生态环境。因粉煤灰颗粒细、表面积大,常将其与煤矸石混合用于重构矿区土壤,但养分释放较慢。土壤微生物参与养分元素的循环,且对环境的变化响应迅速。浇灌木醋液能够促进养分的释放,但对微生物群落的影响目前还不太清晰。本研究以煤矸石与生土混合的基质为研究对象,添加0%、10%、20%和40%(CK、F10、F20、F40)的粉煤灰,再分别浇灌木醋液和蒸馏水。培养3个月后,测定基质理化性质和微生物群落特征,以探究浇灌木醋液和添加粉煤灰对基质微生物群落的影响。结果表明:(1)相较于浇灌蒸馏水,浇灌木醋液显著提高了基质总磷脂脂肪酸(TPLFAs)、总细菌、总真菌、广义细菌、革兰氏阳性菌、革兰氏阴性菌、腐生真菌和厌氧菌含量以及真菌/细菌(F/B),但降低了丛枝菌根真菌、放线菌含量。(2)添加粉煤灰显著提高了基质总PLFAs、总细菌和总真菌含量;F/B在F20和F40处理时显著升高,F10处理的革兰氏阳性菌/革兰氏阴性菌显著低于F20和F40处理,而直链饱和脂肪酸/单不饱和脂肪酸在F10处理显著高于F20和F40处理。(3)浇灌木醋液对基质微生物群落结构的影响效应大于添加粉煤灰。(4)基质水溶性有机碳、全氮、总有机碳和易氧化碳含量是影响基质微生物群落结构的主要理化指标。总之,浇灌木醋液和添加10%～20%粉煤灰提高了微生物生物量,改善了微生物群落结构特征,有利于煤矸石和粉煤灰重构土壤质量的提高。     

敌敌畏杀虫剂对桃树叶际微生物群落结构的影响

采用平板计数法和磷脂脂肪酸（PLFA）分析方法评价了喷施敌敌畏杀虫剂后对桃树叶际微生物群落的影响。平板计数法分析结果表明,经80%敌敌畏乳油的1000倍液喷雾处理后,可培养微生物数量低于喷水对照。PLFA分析结果显示,桃树叶际真菌标记物18：1ω9t磷脂脂肪酸（PLFAs）含量最高,超过总PLFAs含量的60%;喷施杀虫剂后,叶际微生物PLFAs的含量、种类均有所增加,明显有别于喷水对照;并且增加敌敌畏处理次数会增强其对叶际微生物群落影响的显著性。PLFAs主成分分析表明,处理1d后不同样品的叶际微生物群落结构差异最明显,7d后,不同处理样品的叶际微生物群落结构差异变小。