应用磷脂脂肪酸和聚合酶链式反应-变性梯度凝胶电泳分析技术研究湿地植物根际微生物群落多样性

以天津大学校内两个相邻的小型湖泊(青年湖和爱晚湖)为研究区域, 通过采样分析, 利用磷脂脂肪酸(PLFA)和聚合酶链式反应-变性梯度凝胶电泳(PCR-DGGE)分析技术, 研究了湿地植物种类(芦苇(Phragmites australis)和东方香蒲(Typha orientalis))和生长方式(单生和混生)对根际微生物生物量和群落结构的影响。PLFA分析结果表明, 植物根际微生物生物量大于非根际(爱晚湖芦苇除外); 植物种间的差异较大, 东方香蒲根际沉积物中微生物生物量大于芦苇根际; 种内根际微生物受植物的生长状况影响较大, 采样期间两个湖泊中东方香蒲的生长状况(株高)相似, 根际微生物生物量相差不大, 而爱晚湖芦苇由于与东方香蒲共生, 受到东方香蒲的抑制, 使得根际微生物生物量明显低于单独生长的芦苇; 革兰氏阳性细菌数量小于革兰氏阴性细菌的数量, 且根际的革兰氏阳性细菌与革兰氏阴性细菌的比值小于非根际。沉积物中的细菌群落结构主要与植物种类有关, 同一种植物的根际细菌群落结构差异较小(这些根际细菌聚为一类); 不同植物的根际细菌群落结构差异较大。     

蚂蚁筑巢对西双版纳热带森林土壤微生物生物量碳及熵的影响

蚂蚁筑巢能够改变热带森林土壤理化环境,从而对土壤微生物生物量碳及熵的时空动态产生重要影响.本研究以西双版纳高檐蒲桃热带森林群落为对象,采用氯仿熏蒸法对蚂蚁巢地和非巢地土壤微生物生物量碳及熵时空动态进行测定.结果表明: 1)蚁巢地平均微生物生物量碳及熵(1.95 g·kg^-1,6.8%)显著高于非巢穴(1.76 g·kg^-1,5.1%);蚁巢地和非蚁巢地土壤微生物生物量碳呈单峰型时间变化趋势,而土壤微生物熵呈“V”型变化格局.2)蚁巢地和非巢地土壤微生物生物量碳及熵均具有明显的垂直变化:微生物生物量碳随土层加深显著降低,微生物熵则沿土层加深显著升高,但蚁巢微生物生物量碳及熵的垂直变化较非巢穴显著. 3)蚂蚁筑巢引起了巢内水分和温度的显著改变,进而影响土壤微生物生物量碳及熵的时空动态.土壤水分分别解释微生物生物量碳及熵的66%～83%和54%～69%,而土壤温度分别解释土壤微生物生物量碳及熵的71%～86%和67%～76%. 4)蚂蚁筑巢引起土壤理化性质变化对土壤微生物生物量碳和熵产生重要影响.蚁巢土壤微生物生物量碳与土壤有机碳、温度、全氮、含水率呈极显著正相关,与容重、硝态氮,水解氮呈显著正相关,与土壤pH呈极显著负相关;除土壤微生物熵与pH呈显著正相关外,与其他土壤理化指标均呈显著负相关.土壤总有机碳、全氮和温度对微生物生物量碳的贡献最大,而土壤总有机碳和全氮对微生物熵的负作用最小.因此,蚂蚁筑巢能够显著改变微生境(如土壤水分与温度)及土壤理化性质(如总有机碳及全氮),进而调控热带森林土壤微生物生物量碳及熵的时空动态.     

青稞根腐病对根际土壤微生物及酶活性的影响

选取甘肃省卓尼县青稞种植区为研究地点,调查青稞根腐病的发病情况,并分别采集其健康植株和发病株根际的土壤,对比分析其土壤微生物生物量(碳、氮、磷)、微生物数量(细菌、真菌、放线菌)以及过氧化氢酶、蔗糖酶、脲酶、碱性磷酸酶、纤维素酶5种酶活性。结果发现,研究区10个采样点均有青稞根腐病的发生,发病率在5%—20%之间,不同地点发病率不同。根腐病的发生,会显著影响青稞根际微生物生物量,导致微生物生物量碳、氮、磷的含量发生变化,其中微生物生物量氮和磷含量整体降低,且不同采样点微生物量不同。土壤微生物数量总体呈现细菌放线菌真菌的趋势,但不同微生物对根腐病发病的响应不同,细菌和放线菌数量因根腐病的发生而减少,真菌的数量则增多;不同采样点土壤微生物数量不相同,细菌和真菌呈现区域性特征,放线菌的数量不呈现地域性。根腐病的发生还造成土壤酶活性的改变,其中蔗糖酶、脲酶、磷酸酶的含量因根腐病的发生而降低,而纤维素酶则升高,过氧化氢酶的变化没有规律。总而言之,根腐病的发生会使青稞根际土壤微生物组成发生改变,碳、氮、磷等物质代谢受到抑制,而能量代谢发生紊乱。因此,研究和防治青稞根腐病就必须重视土壤微生物及土壤酶的作用。     

岷江干旱河谷造林对土壤微生物群落结构的影响

为了探讨不同造林时间和立地条件对土壤微生物群落结构的影响,采用磷脂脂肪酸(PLFAs)法测定了岷江干旱河谷地区不同造林时间(2002、2006和2011年)及不同立地条件(退耕地和宜林荒山地)营建的岷江柏人工林土壤微生物生物量及群落结构的变化情况。结果表明:由于造林时间较短,不同造林时间的人工林间土壤化学性质没有差异,但土壤微生物生物量和各菌群生物量差异显著,且随着造林时间的增加而增加。不同立地条件下则表现为退耕还林地土壤微生物生物量和各菌群生物量较高。说明土壤微生物对外界因素变化的反映更灵敏。相关性分析结果显示土壤全氮含量与土壤微生物生物量及各菌群生物量显著相关,是影响土壤微生物群落结构的关键因素。     

Soil ecological interactions: comparisons between tropical and subalpine forests

Soil fauna can influence soil processes through interactions with the microbial community. Due to the complexity of the functional roles of fauna and their effects on microbes, little consensus has been reached on the extent to which soil fauna can regulate microbial activities. We quantified soil microbial biomass and maximum growth rates in control and fauna-excluded treatments in dry and wet tropical forests and north- and south-facing subalpine forests to test whether soil fauna effects on microbes are different in tropical and subalpine forests. Exclusion of fauna was established by physically removing the soil macrofauna and applying naphthalene. The effect of naphthalene application on the biomass of microbes that mineralize salicylate was quantified using the substrate induced growth response method. We found that: (1) the exclusion of soil fauna resulted in a higher total microbial biomass and lower maximum growth rate in the subalpine forests, (2) soil fauna exclusion did not affect the microbial biomass and growth rate in the tropical forests, and (3) the microbial biomass of salicylate mineralizers was significantly enhanced in the fauna-exclusion treatment in the tropical wet and the south-facing subalpine forests. We conclude that non-target effects of naphthalene on the microbial community alone cannot explain the large differences in total microbial biomass found between control and fauna-excluded treatments in the subalpine forests. Soil fauna have relatively larger effects on the microbial activities in the subalpine forests than in tropical dry and wet forests.     

长期培肥黑土微生物量磷动态变化及影响因素

长期采用两种不同量有机肥(M2、M4)、化肥(NPK)方式培肥黑土,研究微生物量P在作物生长季动态变化．结果表明。施用有机肥微生物量P显著高于施用化肥(NPK)和不施肥(CK),微生物量P分别为M48．75～47．68mg·kg^-1,M2 3．02～37．16mg·kg^-1,NPK1．59～10．62mg·kg^-1,CK0．76～6．74mg·kg^-1之间,波动性较大．M4、M2处理微生物量P最大值出现在抽雄吐丝期,NPK、CK处理最大值出现在大喇叭口期;施肥数量和种类不同所引起的黑土微生物量P的差异并未因季节变化及玉米生育时期影响而明显改变．微生物量P的动态变化与绝大多数黑土生物、理化特性指标的动态变化没有显著的相关性;微生物量P与黑土生物、理化特性(除全钾外),植物氮、磷、钾含量有极显著的正相关关系,与黑土含水量呈显著正相关关系．     

Dynamics of soil microbial biomass N under zero and shallow tillage for spring wheat,using15N urea

Summary Field studies to determine the effect of zero and shallow (10 cm) cultivation on microbial biomass were conducted on several Chernozemic soils in western Canada. Using the CHCl₃ fumigation method, the distribution of microbial biomass N and the immobilization and subsequent release of added¹⁵N (¹⁵N-urea) from the microbial biomass were determined in the A horizon, at the 0 to 5 and 5 to 10 cm depth, during the growing season for spring wheat.Temporal variation in microbial biomass N, associated with the development of the rhizosphere, was characterized by an increase between Feekes stage 1 and 5 or 10 and decrease at Feekes stage 11.4. Over the long term, the variation in biomass N between tillage systems corresponded with crop residue distribution. Immobilization of fertilizer N was related to the increase in biomass N from Feekes stage 1, which in turn, was associated with the incorporation of recent crop residues or levels of labile organic matter in the surface soil. The study demonstrated the relatively rapid remineralization of immobilized fertilizer N under field conditions and emphasized the role of the microbial biomass N as both a sink and source of mineral N.     

Grass species and soil type effects on microbial biomass and activity

We evaluated plant versus soil type controls on microbial biomass and activity by comparing microbial biomass C, soil respiration, denitrification potential, potential net N mineralization and nitrification in different soils supporting four grass species, and by growing a group of 10 different grass species on the same soil, in two experiments respectively. In the first experiment, none of the microbial variables showed significant variation with grass species while all variables showed significant variation with soil type, likely due to variation in soil texture. In the second experiment, there were few significant differences in microbial biomass C among the 10 grasses but there were significant relationships between variation in microbial biomass C and potential net N mineralization (negative), soil respiration (positive) and denitrification (positive). There was no relationship between microbial biomass C and either plant yield or plant N concentration. The results suggest that 1) soil type is a more important controller of microbial biomass and activity than grass species, 2) that different grass species can create significant, but small and infrequent, differences in microbial biomass and activity in soil, and 3) that plant-induced variation in microbial biomass and activity is caused by variation in labile C input to soil.     

Municipal solid waste compost dose effects on soil microbial biomass determined by chloroform fumigation-extraction and DNA methods

We evaluated the relationship between microbial biomass C and N (B_C and B_N) as estimated by the chloroform fumigation-extraction (CFE) method and microbial biomass DNA concentration in a loam-clayey wheat cultivated soil. The soil received municipal solid waste compost at rates of 40 or 80 t ha^?1 and farmyard manure at 40 t ha^?1. Microbial biomasses C and N and DNA concentration centration showed the highest values for microorganisms counts with compost and farmyard manure at 40 t ha^?1. Compost applications at 40 t ha?1 improve the micro-organisms growth than that of 80 t ha^?1. Moreover a significant decrease of soil microbial biomass was noted after fertilisation for three years. The presence of humic acid and proteins impurities in DNA extracts; even in important level as in F-treated soil; did not affect the microbial biomass. The decrease of microbial biomass was due to heavy metals content elevation in compost at 80 t ha^?1 treated soil. Thus the highest rate of municipal solid waste compost induced the lowest ratio of biomass C to soil organic carbon and the lowest ratio of biomass N to soil organic nitrogen. There was a positive relationship between B_C, B_N and DNA concentration. DNA concentration was significantly and positively correlated with B_C and with B_N. However there was a negative correlation between either micro-organisms numbers and DNA concentration, or B_C and B_N. The comparison of the two used methods DNA extraction and CFE showed the lowest coefficient of variation (cv %) with DNA extraction method. This last method can be used as an alternative method to measure the microbial biomass in amended soils.     

Changes in Soil Microbial Biomass and Residual Indices as Ecological Indicators of Land Use Change in Temperate Permanent Grassland

The relationship between microbial biomass, residues and their contribution to microbial turnover is important to understand ecosystem C storage. The effects of permanent grassland (100 % ryegrass—PG), conversion to modified grassland (mixture of grass and clover—MG) or maize monoculture (MM) on the dynamics of soil organic C (SOC), microbial biomass, fungal ergosterol and microbial residues (bacterial muramic acid and fungal glucosamine) were investigated. Cattle slurry was applied to quantify the effects of fertilisation on microbial residues and functional diversity of microbial community across land use types. Slurry application significantly increased the stocks of microbial biomass C and S and especially led to a shift in microbial residues towards bacterial tissue. The MM treatment decreased the stocks of SOC, microbial biomass C, N and S and microbial residues compared with the PG and MG treatments at 0–40 cm depth. The MM treatment led to a greater accumulation of saprotrophic fungi, as indicated by the higher ergosterol-to-microbial biomass C ratio and lower microbial biomass C/S ratio compared with the grassland treatments. The absence of a white clover population in the PG treatment caused a greater accumulation of fungal residues (presumably arbuscular mycorrhizal fungi (AMF), which do not contain ergosterol but glucosamine), as indicated by the significantly higher fungal C-to-bacterial C ratio and lower ergosterol-to-microbial biomass C ratio compared with the MG treatment. In addition to these microbial biomass and residual indices, the community level physiological profiles (CLPP) demonstrated distinct differences between the PG and MG treatments, suggesting the potential of these measurements to act as an integrative indicator of soil functioning.     

喀斯特地区三种人工林土壤微生物群落结构特征

为揭示不同人工植被修复模式对喀斯特土壤微生物群落的影响,采用氯仿熏蒸提取法和磷脂脂肪酸(phospholipid fatty acid, PLFA)法研究人工构建的降香黄檀(Dalbergia odorifera)纯林(PDOP)、顶果木(Acrocarpus fraxinifolius)纯林(PAFP)、顶果木×降香黄檀混交林(MADP)对土壤微生物生物量及土壤微生物群落结构的影响。结果表明:(1)PDOP的土壤微生物生物量碳(MBC)和微生物生物量氮(MBN)含量显著高于PAFP和MADP,PAFP显著高于MADP。(2)三种人工林土壤真菌、丛枝菌根真菌和总PLFA含量无显著差异,但PDOP土壤细菌、放线菌、丛枝菌根真菌和总PLFA含量均高于PAFP和MADP,PAFP高于MADP。PDOP的土壤细菌、革兰氏阳性菌、革兰氏阴性菌、放线菌的PLFA含量显著高于MADP。MADP的真菌细菌比显著高于PDOP,但与PAFP无显著差异。(3)冗余分析表明,土壤阳离子交换量、pH和C:N是影响土壤微生物群落组成的最主要影响因子。从三种人工林的土壤微生物生物量及微生物群落结构来看,在喀斯特地区MADP并未显示出酸性土地区混交林提高土壤微生物生物量、改善土壤微生物群落结构的优势,但混交林的真菌细菌比最高,更有利于提高土壤生态系统的稳定性。     

亚热带毛竹林土壤磷组分和微生物对施氮的响应

磷(P)是植物和微生物生长的重要营养元素,亚热带地区土壤P有效性较低,且长期高氮(N)沉降可能会造成土壤P有效性进一步降低。本试验开展于戴云山毛竹林,分析了施N 3年对土壤的基本理化性质、P组分、微生物生物量和酸性磷酸单酯酶活性的影响。结果表明: 施N显著增加了土壤NO₃^--N含量,提高了土壤N有效性,但显著降低了易分解态有机磷占全磷的比例,且总有机碳与总有机P的比例>200。土壤微生物生物量碳、微生物生物量磷、酸性磷酸单酯酶活性、微生物生物量碳/微生物生物量磷和微生物生物量氮/微生物生物量磷随施N量的增加而增加。此外,易分解态有机磷占总磷比例与微生物生物量磷呈显著负相关关系。因此,施N加剧了土壤P有效性限制,提高了微生物对P的需求。     

青藏高原东缘高山森林-苔原交错带土壤微生物生物量碳、氮和可培养微生物数量的季节动态

为了了解青藏高原东缘高山森林-苔原交错带土壤微生物的特征和季节变化, 研究了米亚罗鹧鸪山原始针叶林、林线、树线、密灌丛、疏灌丛和高山草甸土壤微生物生物量碳(MBC)、氮(MBN)和可培养微生物数量的季节动态。结果表明, 植被类型和季节动态对MBC、MBN和微生物数量都有显著影响。不同时期的微生物在各植被类型间分布有差异, 植物生长季初期和生长季中期, 树线以上群落的MBC高于树线下的群落, 而到生长季末期恰恰相反, 暗针叶林、林线和树线的MBC显著升高, 各植被之间MBC的差异减小; 微生物数量基本上也是以树线为界, 树线以下群落土壤微生物数量显著低于树线以上群落, 其中密灌丛的细菌数量最高; 可培养微生物数量为生长季末期>生长季初期>生长季中期。生长季末期真菌数量显著增加, 且MBC/MBN最高。统计分析表明, MBN与细菌、真菌、放线菌数量存在显著的相关关系, 而MBC仅与真菌数量存在显著相关关系( p < 0.05)。植物生长季末期大量的凋落物输入和雪被覆盖可能是微生物季节变异的外在因素, 而土壤微生物和高山植物对有效氮的竞争可能是微生物季节变异的内在因素。植物生长季初期对氮的吸收和土壤微生物在植物生长季末期对氮的固定加强了高山生态系统对氮的利用。气候变暖可能会延长高山植物的生长季, 增加高山土壤微生物生物量, 加速土壤有机质的分解, 进而改变高山土壤碳的固存速率。     

全球森林土壤微生物生物量碳氮磷化学计量的季节动态

土壤微生物生物量在森林生态系统中充当具有生物活性的养分积累和储存库。土壤微生物转化有机质为植物提供可利用养分, 与植物的相互作用维系着陆地生态系统的生态功能。同时, 土壤微生物也与植物争夺营养元素, 在季节交替过程和植物的生长周期中呈现出复杂的互利-竞争关系。综合全球数据对温带、亚热带和热带森林土壤微生物生物量碳(C)、氮(N)、磷(P)含量及其化学计量比值的季节动态进行分析, 发现温带和亚热带森林的土壤微生物生物量C、N、P含量均呈现夏季低、冬季高的格局。热带森林四季的土壤微生物生物量C、N、P含量都低于温带和亚热带森林, 且热带森林土壤微生物生物量C含量、N含量在秋季相对最低, 土壤微生物生物量P含量四季都相对恒定。温带森林的土壤微生物生物量C:N在春季显著高于其他两个森林类型; 热带森林的土壤微生物生物量C:N在秋季显著高于其他2个森林类型。温带森林土壤微生物生物量N:P和C:P在四季都保持相对恒定, 而热带森林土壤微生物生物量N:P和C:P在夏季高于其他3个季节。阔叶树的土壤微生物生物量C含量、N含量、N:P、C:P在四季都显著高于针叶树; 而针叶树的土壤微生物生物量P含量在四季都显著高于阔叶树。在春季和冬季时, 土壤微生物生物量C:N在阔叶树和针叶树之间都没有显著差异; 但是在夏季和秋季, 针叶树的土壤微生物生物量C:N显著高于阔叶树。对于土壤微生物生物量的变化来说, 森林类型是主要的显著影响因子, 季节不是显著影响因子, 暗示土壤微生物生物量的季节波动是随着植物其内在固有的周期变化而变化。植物和土壤微生物密切作用表现出来的对养分的不同步吸收是保留养分和维持生态功能的一种权衡机制。     

Flux and turnover of fixed carbon in soil microbial biomass of limed and unlimed plots of an upland grassland ecosystem

The influence of liming on rhizosphere microbial biomass C and incorporation of root exudates was studied in the field by in situ pulse labelling of temperate grassland vegetation with (13)CO(2) for a 3-day period. In plots that had been limed (CaCO(3) amended) annually for 3 years, incorporation into shoots and roots was, respectively, greater and lower than in unlimed plots. Analysis of chloroform-labile C demonstrated lower levels of (13)C incorporation into microbial biomass in limed soils compared to unlimed soils. The turnover of the recently assimilated (13)C compounds was faster in microbial biomass from limed than that from unlimed soils, suggesting that liming increases incorporation by microbial communities of root exudates. An exponential decay model of (13)C in total microbial biomass in limed soils indicated that the half-life of the tracer within this carbon pool was 4.7 days. Results are presented and discussed in relation to the absolute values of (13)C fixed and allocated within the plant-soil system.     

退化高寒草甸土壤微生物及酶活性特征

采用Biolog等方法,分析不同退化程度(未退化ND、轻度退化LD、中度退化MD、重度退化SD和黑土滩ED)高寒草甸0～10和10～20 cm土层土壤微生物量碳氮、碳代谢指纹和酶活性.结果表明: 所有草甸土壤微生物量、多样性指数和蔗糖酶活性在0～10 cm土层均显著高于10～20 cm土层,0～10 cm土层脲酶活性则显著低于10～20 cm土层.土壤微生物量C/N随草地退化程度加重显著降低.0～10 cm土层,ND和LD微生物量碳、氮均显著高于其他草地,MD、SD和ED微生物量碳无显著差异,MD微生物量氮显著低于其他草地;平均颜色变化率(AWCD)和McIntosh指数(U)随草地退化程度加重曲线下降,ND与MD间差异显著,其他草地间无显著差异;Shannon指数(H)和Simpson指数(D)在不同草地间均无显著差异;MD和SD脲酶活性最高,ED磷酸酶和蔗糖酶活性最低,与其他草地相比均差异显著.10～20 cm土层,ND和LD微生物量碳显著高于其他草地,MD、SD和ED间无显著差异,LD和ED微生物量氮显著高于其他草地,ND和SD间差异不显著;MD碳代谢指数最低,与LD和SD相比差异显著,ND和LD的AWCD和U指数均显著高于ED,H指数和D指数在ND、LD、SD和ED间差异不显著;ND和MD脲酶活性显著高于其他草地,LD、SD和ED间无显著差异;MD磷酸酶活性最高,与LD、SD和ED相比差异显著;MD蔗糖酶活性显著低于其他草地,ND、LD、SD和ED间差异不显著.不同退化程度高寒草地的地下生物量均与微生物量、碳代谢指数和磷酸酶呈显著正相关;脲酶与微生物量氮、H指数和D指数呈显著负相关.     

武夷山植被带土壤微生物量沿海拔梯度的变化

土壤微生物量是陆地生态系统碳循环的重要组成部分,在森林生态系统物质循环和能量转化中占有特别重要的地位.以武夷山常绿阔叶林(EBF)、针叶林(CF)、亚高山矮林(DF)和高山草甸(AM)为试验对象,研究了土壤微生物量沿海拔梯度的变化特征.结果表明:在0～10cm土壤层,随着海拔高度的增加,年平均土壤微生物量增大,AM的年平均土壤微生物量为4.07 g·kg-1,分别为DF、CF和EBF的2.06、3.21倍和3.91倍;AM的年平均土壤微生物量显著大于DF、CF和AM(p<0.01),DF的年平均土壤微生物量显著大于EBF、CF(p<0.05),EBF和CF的年平均土壤微生物量无显著性差异(p>0.05),10～25cm土壤层的年平均土壤微生物量的变化规律与上层基本一致;在0～10cm土壤层,不同海拔年平均土壤微生物量分别与土壤有机碳、全氮、全硫含量以及土壤湿度呈显著正相关(p<0.05),在10～25cm土壤层,不同海拔年平均土壤微生物量分别与土壤有机碳、全氮含量呈显著正相关(p<0.05).研究表明,武夷山亚热带森林年平均土壤微生物量随海拔高度升高而增加,土壤有机碳、全氮、全硫和土壤湿度可能是调控土壤微生物量沿海拔梯度变化的主要因子.     

Abundance, biomass, structure, and activity of the microbial complexes of minerotrophic and ombrotrophic peatlands

Very large microbial biomass was revealed in peat bogs by means of fluorescence microscopy. In ombrotrophic peatlands, the pool of the dry-weight microbial biomass in the 1.5-m layer constituted 3-4 t/ha and was twice as high as in the minerotrophic peat bogs. Fungal biomass was predominant (55-99%) in ombrotrophic peatlands, while bacterial biomass predominated in minerotrophic peatlands (55-86%). In ombrotrophic peatlands, the microbial biomass was concentrated in the upper layers, while in minerotrophic peatlands, it was uniformly distributed in the bulk. After drainage, the microbial pool in the ombrotrophic peatlands increased twofold; that in the minerotrophic peatlands remained at the same level. The potential activity of nitrogen fixation and denitrification was revealed across the whole profile of the peatlands. The average values of these potential activities were five times higher in the minerotrophic peatlands, where bacterial biomass predominated.     

Effects of land use pattern on soil microbial biomass carbon in Xishuangbanna

In January 2006 - September 2007, a controlled litter-removal and root-cutting experiment was conducted to study the effects of different land use patterns (secondary forest or rubber plantation) on soil microbial biomass carbon in Xishuangbanna, China. After the secondary forest converted into rubber plantation, soil nutrient contents and plant carbon input decreased obviously, and soil microbial biomass carbon had a significant decrease. These two forest types had a higher soil microbial biomass carbon in rainy season than in dry season. In secondary forest, soil microbial biomass carbon was significantly positively correlated with soil temperature; while in rubber plantation, the microbial biomass carbon was positively correlated with soil moisture. In secondary forest, soil microbial biomass carbon was controlled by the nutrient inputs from plant roots, but less affected by litter amount. Also in secondary forest, soil microbial biomass carbon was significantly positively correlated with fine-root biomass and its C and N inputs. In rubber plantation, both the fine-root biomass and its C and N inputs and the litter amount had lesser effects on soil microbial biomass carbon. These results suggested that planting rubber induced the decreases of soil nutrient contents and pH value, and, added with serious artificial disturbances, reduced the soil microbial biomass carbon and changed its controlling factors, which in turn would affect other soil ecological processes.     

一种利用Profile-1生物发光仪快速测定土壤中微生物量的改良方法

开发了一种利用Profile-1生物发光仪测定土壤中微生物量的改良方法,并以此方法分别测定了标准大肠杆菌茵液以及3种不同类型的土壤(九段沙湿地土壤,崇明东滩大田土壤和崇明实验地改良土壤)的微生物量,并将结果与Profile-1生物发光仪自带的标准分析方法以及传统的菌落计数法进行比较。结果显示,改良的ATP提取方法(BAB改良分析法)和Profile-1生物发光仪自带的标准分析方法都可用于液体样品中微生物量的测定,其灵敏度和准确度无显著差异(P0.05)。但在测定土壤样品时,菌落计数法测定结果大约占BAB改良分析法测定结果的1%～5%,占Profile-1生物发光仪自带的标准分析方法的测定结果的22%～99%。这表明在分析土壤样品时,BAB改良分析法较Profile-1生物发光仪自带的标准分析方法的ATP提取效率更高,可显著提高仪器检测土壤样品的灵敏度和可靠性,因此可有效应用于各类土壤的微生物量的监测,为土壤环境监控提供微生物量的可靠数据。