生物炭对温室黄瓜不同连作年限土壤养分和微生物群落多样性的影响

以温室黄瓜连作6年和10年土壤添加质量比为5%生物炭为处理,以不添加生物炭为对照,采用桶栽的方法,研究了生物炭对不同年限连作土壤养分和微生物群落多样性的影响.结果表明: 与连作土壤相比,生物炭处理的连作6年土壤的黄瓜单株产量提高11.4%,连作10年土壤产量提高62.8%.施入生物炭显著降低了2种连作土壤容重,显著提高了有机质、速效磷含量、阳离子交换量(CEC)和pH;显著提高了土壤细菌数量和细菌/真菌,降低了真菌和尖孢镰刀菌数量,使土壤类型由真菌型向细菌型转变,尤其对连作10年土壤作用最为明显,土壤细菌和细菌/真菌分别是未处理的2.00和3.64倍,真菌和尖孢镰刀菌数量分别是未处理的54.8%和55.9%.土壤微生物群落碳源利用分析表明,10年连作土壤施入生物炭可显著提高土壤微生物活性、Shannon指数和均匀度指数,分别是未处理的1.50、2.14和1.31倍,同时显著提高了土壤微生物对糖类、氨基酸类、酚酸类和胺类碳源的利用强度,分别是未处理的1.62、1.81、1.74和1.93倍.相关性分析表明,土壤容重、速效磷含量、CEC和pH 4个指标对微生物群落变化的影响较显著.综上,生物炭通过对连作土壤理化性质及土壤微生物生态系统的改善,优化了黄瓜根区环境,促进了黄瓜产量的提高,缓解了温室黄瓜连作障碍.     

有机物料减轻设施连作黄瓜苗期病害的微生物效应

在黄瓜已感染立枯病、枯萎病的连作土壤上,接种病原菌菌丝,施入3种不同组分有机物料(稻草、木屑、猪粪),分别用1％、2％、3％3种用量研究不同有机物料减轻黄瓜枯萎病、立枯病的效果．结果表明,抗病效果为稻草>猪粪>木屑处理,并随其用量的增加抗病效果更好．土培试验结果表明,增施有机物料后土壤中细菌、氨化细菌、放线菌、真菌数量增加．中稻草和猪粪对土壤微生物区系的影响大于木屑．施用稻草后不仅土壤细菌、真菌数量增加,而且放线菌数量最高,青霉、木霉成为真菌的优势种属．施用猪粪后土壤细菌数最多,以假单孢菌、芽孢杆菌为优势种属,真菌数也增多．木屑处理的细菌、放线菌、真菌数量增加较少,但随着施入时间延长效果增强．     

杉木连栽土壤微生物多样性的比较研究

分析了位于湖南会同广坪镇1～4代人工杉木林根际土壤微生物数量变化情况,结果表明,随杉木连栽代数的增加,根际土壤中三大类群微生物数量发生显著变化,细菌和放线菌数量明显减少,真菌数量显著增加.利用PCR和DGGE技术分析了1～4代杉木林根际土壤细菌区系和真菌区系.结果表明,细菌生物多样性在不同连栽代数杉木根际土壤中变化不明显,各代杉木土壤之间细菌的遗传相似性为87%.而真菌随连栽代数的增加,DGGE图谱带逐渐减少,真菌生物多样性降低,各代杉木土壤之间真菌的遗传相似性也较低,仅为45%.对各代杉木土壤主要真菌类群的分析表明,随连栽代数的增加,病原真菌及产毒真菌增加显著.     

黄瓜连作土壤酚酸类物质积累对土壤微生物和酶活性的影响

伴随连作年限的增加,日光温室黄瓜连作土壤中酚酸类物质(对羟基苯甲酸、阿魏酸、苯甲酸)明显积累,连作5～9年的土壤酚酸类物质含量显著高于连作1～3年的土壤.伴随外源酚酸类物质处理浓度的增加,黄瓜根区土壤中细菌、放线菌和微生物总量以及N生理群均呈先升后降趋势,在80 μg·g^-1处理浓度下细菌、放线菌数量最多,处理浓度在120μg·g^-1以下土壤真菌数量(包括尖孢镰刀菌、疫霉)急剧增长;多酚氧化酶、过氧化氢酶、蔗糖酶、脲酶和蛋白酶活性也同样呈先升后降趋势,但其峰值对应的浓度不同.     

营养基质对连作栽培下温室黄瓜生长及土壤微环境的影响

分别利用营养基质(稻草+田园土壤+膨化鸡粪)及土壤在同一温室内进行黄瓜的槽式连作栽培,研究其对黄瓜生长及土壤微环境的影响.结果表明:随着连作茬次的增加,两种栽培方式均出现了不同程度的连作效应.同一连作茬次间比较,营养基质的养分含量、蔗糖酶和脲酶活性、细菌/真菌均明显高于土壤,而真菌数量低于土壤,营养基质栽培改变了细菌种群结构,促进了黄瓜植株生长及产量提高.相关分析表明,连作栽培条件下土壤细菌数量与黄瓜株高、根干质量呈显著正相关,与地上部干质量及产量呈极显著正相关;土壤脲酶活性与产量呈极显著正相关.综上,与土壤栽培相比,营养基质栽培能够明显改善根区微环境,有效延缓连作障碍的发生.     

施用棉秆炭对新疆连作棉花根际土壤微生物群落结构和功能的影响

以棉秆移除(NPK)和棉秆还田(NPKS)为对照,采用平板计数、Biolog和DGGE等3种方法,研究了棉秆移除基础上施用常量棉秆炭(22.50 t·hm^-2,NPKB-1)和增量棉秆炭(45.00 t·hm^-2,NPKB-2)对新疆连作棉花根际土壤微生物数量、群落功能和结构多样性的影响.结果表明：与NPK和NPKS处理相比,棉秆炭施用显著增加了连作棉田根际土壤中细菌和放线菌数量;NPKB-1处理真菌数量显著高于NPK处理,但增量棉秆炭NPKB-2处理与NPK处理差异不显著;2个棉秆炭处理的真菌数量均低于NPKS处理.棉秆炭处理AWCD值较高,显著提高了微生物丰富度指数,可促进利用糖类、氨基酸类和羧酸类碳源的微生物生长,尤其是利用与根系分泌物相关的酚酸类碳源的微生物.DGGE电泳结果表明,施用棉秆炭(尤其是增量棉秆炭)后,土壤细菌DGGE图谱条带数增多,增加了土壤中芽单胞菌门、酸杆菌门、变形菌门和放线菌门中一些菌群的丰度.UPGMC聚类分析表明,NPKB-2处理明显区别于其他处理,而NPKS、NPK和NPKB-1处理细菌群落结构相似.表明高量施用棉秆炭可显著提高棉花根际土壤微生物多样性,并明显改变土壤细菌群落结构,对连作棉田生态系统健康有改善作用.     

不同蔬菜与番茄轮作对设施土壤微生物多样性、酶活性及土壤理化性质的影响

【目的】番茄是一种受连作障碍影响明显的蔬菜作物,本试验旨在研究不同蔬菜作物与番茄轮作后对设施土壤微生物多样性、酶活性及土壤理化性质的影响,以期筛选出适宜与番茄轮作的蔬菜作物,为从设施栽培模式选择角度缓解或避免番茄连作障碍提供理论依据。【方法】试验以连续两茬种植番茄后分别种植大白菜(A)、黄瓜(B)、辣椒(C)、茄子(E)、秋葵(F)、西葫芦(G)6种作物为不同处理,以继续种植番茄(D)和休耕闲置土壤(H)为对照,采用16S rRNA和真菌ITS区测序、同时测定土壤酶活性、pH值、有机质含量、速效氮、磷、钾含量,研究不同蔬菜作物与番茄轮作对土壤微生物多样性、酶活性及土壤理化性质的影响。【结果】种植作物土壤细菌和真菌多样性指数均显著高于闲置土壤(H);番茄连作与轮作土壤中的细菌门水平群落结构比较固定,但不同物种的丰度差异较大。真菌对于环境变化的响应比细菌更加敏感,轮作各样本间真菌群落结构差异明显大于细菌群落结构,在物种丰度和门水平上均存在较大差异;轮作茄子和大白菜显著增加了土壤中硝化细菌[亚硝化单胞菌属(Nitrosomonas)、亚硝化螺菌属(Nitrosospira)]的丰度;PCA分析表明轮作茄子和空白闲置土壤细菌和真菌的群落结构与其他处理的差异较大;轮作不同作物土壤酶活性差异显著,但变化规律不明显。轮作大白菜、黄瓜和空白闲置土壤过氧化氢酶活性显著高于番茄连作和轮作其他作物。不同蔬菜轮作土壤肥力主成分分析结果表明土壤pH值、有机质、速效氮与速效磷是主要贡献因子,综合肥力排名第一的为空白土样,其次为轮作黄瓜的土样,综合肥力最低的为轮作茄子土样。【结论】种植作物可以显著提高土壤微生物多样性;轮作茄子和大白菜显著增加了土壤中硝化细菌的丰度,有利于土壤中氮素代谢和利用;轮作黄瓜和大白菜,显著提高土壤中过氧化氢酶的活性,有利于降低番茄连作产生的自毒作用。因此综合分析认为,茄子、黄瓜和大白菜是避免或缓解番茄连作障碍的潜在优势轮作作物。     

日光温室连作黄瓜根区微生物区系及酶活性的变化

以日光温室黄瓜连作土壤为研究对象,研究不同连作年限根区土壤微生物数量、种类及酶活性的变化,并运用通径分析方法阐明其与土壤主要理化性状的关系,结果表时,土壤微生物数量、酶活性表现明显的温室连作将就;伴随连作年限的增加,土壤微生物总量、细菌、放线菌数均呈倒“马鞍”形变化,真菌数量则呈线性增长、微生物由“细菌型”向“真菌型”过渡,其中氨化细菌和尖孢镰刀菌分别为温室黄瓜连作土壤的优势细菌和真菌生理群;多数土壤酶活性的变化也呈现倒“马鞍”形,通径分析表明,佩量元素（Cu、Mn、Fe)、有机质、速效N、容重为温室连作土壤微生物区系及酶活性的主要影响因素。     

轮作与休闲对日光温室黄瓜连作土壤微生物和酶活性的影响

采用盆栽试验,研究了不同作物轮作和休闲方式对日光温室黄瓜连作土壤微生物数量、酶活性及后茬黄瓜生长和产量的影响.结果表明： 与连作相比,轮作有利于改善土壤微生物结构,增加细菌和放线菌数量,减少真菌数量;轮作与休闲有利于提高土壤转化酶、脲酶、过氧化氢酶和多酚氧化酶活性.在不同作物轮作和休闲方式下,后茬黄瓜结果期的细菌、放线菌数量和土壤转化酶活性均呈先升后降趋势,在盛瓜期达到最大值;真菌数量随生育期延长而增加;脲酶、过氧化氢酶和多酚氧化酶活性则随生育期延长而降低,在初瓜期最高.不同栽培模式下,以大葱-黄瓜轮作和糯玉米-黄瓜轮作的效果更佳,明显改善了后茬黄瓜的生长,提高了产量.     

葡萄连作对土壤细菌和真菌种群的影响

分别采集种植葡萄30年的连作园和3年的新植园根围土、非根围土及葡萄园周边的空地土壤,采用PCR DGGE技术,研究葡萄连作对土壤细菌和真菌种群结构及多样性的影响,并对分离出的优势种扩增条带进行测序.结果表明：葡萄连作后土壤细菌和真菌的多样性增加,且根围土壤的微生物多样性高于非根围土壤.聚类分析显示：葡萄长期连作后根围与非根围土壤细菌和真菌的种群结构趋于一致,两者不同于空地土壤;而短期种植葡萄的根围土壤细菌和真菌的种群结构不同于非根围土壤和空地土壤.与新植园相比,连作园根围土壤中微生物种群结构发生较大变化,细菌中Flavobacterium sp.（DQ339585）和Bacillus sp.（AY039821）种群数量减少,Pedobacter sp.（AJ871084）种群数量增多;真菌中Omphalina farinolens（EF413029）出现,Pestalotiopsis sp.(DQ657877,DQ657875,DQ657871）、Phacidium lacerum（DQ470976）和Lecythophora decumbens（AF353597）种群数量减少,Pilidium acerinum voucher（AY48709）种群数量增多.其中Bacillus sp.、Flavobacterium sp.和Pestalotiopsis sp.对病原菌具有颉颃作用,连作园根围土中上述微生物种群数量的减少,不利于葡萄对病原菌的颉颃;Pilidium acerinum voucher数量的增加可能与葡萄连作后病害加重有关.     

植物、土壤及土壤管理对土壤微生物群落结构的影响

土壤微生物是土壤生态系统的重要组成部分,对土壤微生物群落结构多样性的研究是近年来土壤生态学研究的热点。本文综述了有关植物、土壤类型以及土壤管理措施对土壤微生物群落结构影响的最新研究结果,指出植物的作用因植物群落结构多样性、植物种类、同种植物不同的基因型,甚至同一植物不同根的区域而异;而土壤的作用与土壤质地和有机质含量等因素有关;植物和土壤类型在对土壤微生物群落结构影响上的作用存在互作关系。不同的土壤管理措施对土壤微生物群落结构影响较大,长期连作、大量的外援化学物质的应用降低了土壤微生物的多样性;而施用有机肥、免耕可以增加土壤微生物群落结构多样性,有利于维持土壤生态系统的功能。     

Estimating respiration of roots in soil: Interactions with soil CO2, soil temperature and soil water content

Little information is available on the variability of the dynamics of the actual and observed root respiration rate in relation to abiotic factors. In this study, we describe I) interactions between soil CO₂ concentration, temperature, soil water content and root respiration, and II) the effect of short-term fluctuations of these three environmental factors on the relation between actual and observed root respiration rates. We designed an automated, open, gas-exchange system that allows continuous measurements on 12 chambers with intact roots in soil. By using three distinct chamber designs with each a different path for the air flow, we were able to measure root respiration over a 50-fold range of soil CO₂ concentrations (400 to 25000 ppm) and to separate the effect of irrigation on observed vs. actual root respiration rate. All respiration measurements were made on one-year-old citrus seedlings in sterilized sandy soil with minimal organic material.Root respiration was strongly affected by diurnal fluctuations in temperature (Q₁₀ = 2), which agrees well with the literature. In contrast to earlier findings for Douglas-fir (Qi et al., 1994), root respiration rates of citrus were not affected by soil CO₂ concentrations (400 to 25000 ppm CO₂; pH around 6). Soil CO₂ was strongly affected by soil water content but not by respiration measurements, unless the air flow for root respiration measurements was directed through the soil. The latter method of measuring root respiration reduced soil CO₂ concentration to that of incoming air. Irrigation caused a temporary reduction in CO₂ diffusion, decreasing the observed respiration rates obtained by techniques that depended on diffusion. This apparent drop in respiration rate did not occur if the air flow was directed through the soil. Our dynamic data are used to indicate the optimal method of measuring root respiration in soil, in relation to the objectives and limitations of the experimental conditions.     

Available soil nitrogen in relation to fractions of soil nitrogen and other soil properties

The available N of 27 soils from England and Wales was assessed from the amounts of N taken up over a 6-month period by perennial ryegrass grown in pots under uniform environmental conditions. Relationships between availability and the distribution of soil N amongst various fractions were then examined using multiple regression. The relationship: available soil N (mg kg^–1 dry soil)=(N_min×0.672)+(N_inc×0.840)+(N_mom×0.227)–5.12 was found to account for 91% of the variance in available soil N, where N_min=mineral N, N_inc=N mineralized on incubation and N_mom=N in macro-organic matter. The N mineralized on incubation appeared to be derived largely from sources other than the macro-organic matter because these two fractions were poorly correlated. When availability was expressed in terms of available organic N as % of soil organic N (N_ao) the closest relationship with other soil characteristics was: N_ao=[N_inc×(1.395–0.0347×CN_mom]+[N_mom×0.1416], where CN_mom=CN ratio of the macro-organic matter. This relationship accounted for 81% of the variance in the availability of the soil organic N.The conclusion that the macro-organic matter may contribute substantially to the available N was confirmed by a subsidiary experiment in which the macro-organic fraction was separated from about 20 kg of a grassland soil. The uptake of N by ryegrass was then assessed on two subsamples of this soil, one without the macro-organic matter and the other with this fraction returned: uptake was appreciably increased by the macro-organic matter.     

生物质炭对水稻土团聚体微生物多样性的影响

生物质炭施用对土壤微生物群落结构的影响已有报道,但土壤团聚体粒组中微生物群落对生物质炭施用的响应的研究还相对不足。以施用玉米秸秆生物质炭两年后的水稻土为对象,采用团聚体湿筛法,通过高通量测序对土壤团聚体的微生物群落结构与多样性进行分析,结果表明:(1)与对照相比,生物质炭施用显著促进了大团聚体(2000—250μm)的形成,并提高了团聚体的稳定性。(2)不同粒径团聚体间微生物相对丰度存在显著差异。在未施生物质炭的处理(C0)中,随着团聚体粒径增大,变形菌门、子囊菌门、β-变形杆菌目、格孢腔菌目的相对丰度逐渐降低,而酸杆菌门、担子菌门、粘球菌目、类球囊霉目的相对丰度逐渐升高。(3)生物质炭施用显著改变了团聚体间的微生物群落结构。与C0处理相比,生物质炭施用处理的大团聚体中变形菌门、鞭毛菌门和β-变形杆菌目的相对丰度分别显著提高了14.37%、33.28%和33.82%;微团聚体(250—53μm)中酸杆菌门、子囊菌门和粘球菌目的相对丰度分别显著降低了20.15%、19.93%和17.66%;粉、黏粒组分(53μm)中担子菌门的相对丰度升高90.25%,而子囊菌门和鞭毛菌门的相对丰度分别降低12.15%和12.58%。由此可见,生物质炭不仅改变土壤团聚体组成和分布,同时伴随着土壤微生物群落结构的改变。     

Effect of soil moisture on bioremediation of chlorophenol-contaminated soil

A chlorophenol-contaminated soil was tested for the biodegradability in a semi-pilot scale microcosm using indigenous microorganisms. More than 90% of 4-chlorophenol and 2,4,6-trichlorophenol, initially at 30 mg kg^–1, were removed within 60 days and 30 mg pentachlorophenol kg^–1 was completely degraded within 140 days. The chlorophenols were degraded more effectively under aerobic condition than under anaerobic condition. Soil moisture had a significant effect with the slowest degradation rate of chlorophenols at 25% in the range of 10–40% moisture content. At 25–40%, the rate of chlorophenol degradation was directly related to the soil moisture content, whereas at 10–25%, it was inversely related. Limited oxygen availability through soil agglomeration at 25% moisture content might decrease the degradation rate of chlorophenols.     

耕作方式对潮土土壤团聚体微生物群落结构的影响

为探究不同耕作方式对潮土土壤团聚体微生物群落结构和多样性的影响,采用磷脂脂肪酸(PLFA)法测定了土壤团聚体中微生物群落。试验设置4个耕作处理,分别为旋耕+秸秆还田(RT)、深耕+秸秆还田(DP)、深松+秸秆还田(SS)和免耕+秸秆还田(NT)。结果表明:与RT相比,DP处理显著提高了原状土壤和>5 mm粒级土壤团聚体中真菌PLFAs量和真菌/细菌,为真菌的繁殖提供了有利条件,有助于土壤有机质的贮存,提高了土壤生态系统的缓冲能力;提高了5～2 mm粒级土壤团聚体中细菌PLFAs量,降低了土壤革兰氏阳性菌/革兰氏阴性菌,改善了土壤营养状况;提高了<0.25 mm粒级土壤团聚体中微生物丰富度指数。总的来说,深耕+秸秆还田(DP)对土壤团聚体细菌和真菌生物量有一定的提高作用,并且在一定程度上改善了土壤团聚体微生物群落结构,有利于增加土壤固碳能力和保持土壤微生物多样性。冗余分析结果表明,土壤团聚体总PLFAs量、细菌、革兰氏阴性菌和放线菌PLFAs量与土壤有机碳相关性较强,革兰氏阳性菌PLFAs量与总氮相关性较强。各处理较大粒级土壤团聚体微生物群落主要受碳氮比、含水量、pH值和团聚体质量分数的影响,较小粒级土壤团聚体微生物群落则主要受土壤有机碳和总氮的影响。     

The porosity of soil aggregates from bulk soil and from soil adhering to roots

Summary Total porosity and pore-size distribution (p.s.d.) were determined in soil aggregates taken in plots planted with maize and treated with farmyard manure and three rates of compost. Soil aggregates were collected from the soil adherent to the maize roots (root soil aggregates) and from bulk soil (bulk soil aggregates). Mercury intrusion porosimetry was used to evaluate the total porosity and the p.s.d. Treatments did not affect the total porosity of the bulk soil aggregates. The same was observed for the root soil aggregates. However the total porosity of the root soil aggregates was always lower than that of the bulk soil aggregates. The loss of total porosity was found to be due to a decrease in the percentage of larger pores with respect to the total.     

The breakdown of malathion in soil and soil components

The disappearance of the organophosphorus insecticide, malathion, from a silt loam soil and from its organic and inorganic components was examined. Half-lives and the time taken for 90% decomposition in nonsterile, sodium azide-treated, and 2.5 Mrad-irradiated soils were similar (3/4–1 1/2 days and 4–6 days, respectively) but breakdown in autoclaved soils was negligible. Decay in nonsterile sand, silt, and clay minus organic matter fractions was 3–6 times slower than that recorded in the original soil. Breakdown of malathion in the clay plus organic matter fraction (organo-mineral complex) was rapid (half-life, 1 day), as was the case in the separated organic matter (half-life, 1 3/4 days). Filter-sterilized organic matter was not as effective in catalyzing the breakdown of malathion (half-life, 4 days), and no loss occurred from any of the autoclaved components. Irradiation doses of 2.5 and 5.0 Mrad had little influence on the ability of soil to degrade malathion. Thereafter, increases up to 20 Mrad had a more drastic, though far from totally inhibitory, effect. Our results suggest that either the colloidal organic matter itself, or a fraction associated with it, is the most important single factor concerned with the rapid breakdown of malathion in the soil studied. Direct microbial metabolism is a slower process and may have a significant role in malathion disappearance in coarsetextured soils low in colloidal organic matter. The catalytic component of the organic matter is suggested to be a stable exoenzyme and is supportive of reports by other workers. The quantitative effect of organo-mineral complex (containing the active degradative ingredient) additions to sand and silt fractions on the rate of subsequent malathion decay is also described.