Solid-state C NMR to assess organic matter transformation in a subsurface wetland under cheese-dairy farm effluents

Solid-state ¹³C NMR were used to follow organic matter transformation in a subsurface wetland under the effluent of a small cheese-dairy farm under a Mediterranean climate. The results showed that the ratios commonly used to quantify humification, (aromaticity and Alkyl-C/O-Alkyl-C ratios) can be considered as relevant chemical indicators of organic matter transformation. Polysaccharides were transformed throughout the subsurface wetland whereas aromatic, phenolic and alkyl compounds accumulated. Furthermore, Phenolic-C signal and O-Alkyl-C signal were negatively correlated to proteases and β-galactosidase activities showing that recalcitrant molecules actually accumulated. These results were correlated with high purification yields: the average decrease in chemical demand in oxygen was 90.75% and that in Total Kjeldahl Nitrogen was 75.65%. Thus subsurface wetlands can be considered as an efficient technology to purify effluents with high organic matter contents, such as cheese-dairy effluent, under drastic climate conditions. Furthermore this study highlights the fact that solid-state ¹³C NMR is a suitable tool to follow organic matter transformation.     

Factors limiting microbial activities in soil

Summary The only nutrient element other than nitrogen and phosphorus which limited microbial activity in a sandy soil was sulfur. The addition of extremely small quantities of MgSO₄, ranging from 0.32 to 1.6 mg sulfur/100 g soil, markedly increased the rate of oxidation of glucose. The optimum concentration of sulfur was correlated with the levels of glucose added, and a C/S ratio of 900 or less was required for maximum respiration. A number of compounds containing sulfur at different oxidation stages and in various structural configurations readily satisfied the sulfur requirement, indicating that the response was to sulfur as a nutrient and not to sulfate as an electron acceptor. Thiourea and elemental sulfur were utilized only slightly. The differential utilization of the various sulfur-containing compounds and the implications of sulfur as a limiting factor of microbial activities in soil were discussed.Paper No. 33.     

会仙岩溶湿地4种覆被下土壤酶活性和微生物生物量

研究湿地系统中的稻田被撂荒以后土壤酶活性和微生物生物量的变化可以为湿地的保护提供参考依据。以桂林会仙岩溶湿地为研究样地,采集芦苇湿地、华科拉莎草湿地、稻田撂荒地（以双穗雀稗和莲子草为优势植被）和稻田的耕层土壤样品,采用比色法和氯仿熏蒸法分别检测土壤酶活性和微生物生物量。结果表明,稻田撂荒地的土壤微生物生物量碳（MBC）为（345.20±30.06） mg/kg,显著低于其它三种覆被下的土壤;微生物生物量氮（MBN）、微生物DNA、蔗糖酶活性和碱性磷酸酶活性分别为（48.03±18.48） mg/kg、（5.65±1.48）μg/kg、（19.16±1.43） mg g^-1（24h）^-1和（2.20±0.94） mg g^-1（24h）^-1,均显著低于稻田,而与两种天然湿地没有显著差异。主成分分析表明,稻田撂荒地能与稻田明显分开,而与其它两种覆被土壤有所交叉。统计分析表明,MBC和碱性磷酸酶活性均与pH呈显著正相关关系（P<0.05）;MBN、蔗糖酶活性和碱性磷酸酶活性均与土壤总有机碳（SOC）呈显著的正相关关系（P<0.05）;土壤微生物DNA与SOC、总氮（TN）和碱解氮（AN）均呈显著正相关关系（P<0.01）,与Mg²⁺呈显著正相关关系（P<0.05）。以上研究结果表明,会仙湿地中的稻田在撂荒以后,土壤微生物生物量和两种土壤酶活性显著降低,影响微生物生物量和土壤酶活性变化的主要因素是pH、SOC、TN、AN和Mg²⁺。因此,建议在稻田撂荒地上重新种植水稻,以加快会仙岩溶湿地的恢复过程。     

三江源地区高寒草原土壤微生物活性和微生物量

为了揭示青藏高原高寒草地土壤微生物活性和微生物量碳、氮情况,同时探讨气候变化对土壤微生物的影响,以青藏高原腹地三江源自然保护区高寒草原土壤为研究对象,选择土壤质地、植被类型基本一致,海拔高度不同（3400—4200m）的4个样地,分析测定了土壤微生物（细菌、真菌、放线菌和部分生理功能微生物群）数量、土壤微生物量（碳、氮）、土壤酶（纤维素酶、蛋白酶、脲酶用、蔗糖酶）活性。结果表明：研究区域均含有较丰富的土壤有机碳和养分,微生物数量多少为细菌>放线菌>真菌,主要功能微生物菌群数量为氨化细菌>好气性固氮菌>硝化细菌>亚硝化细菌,样地间的微生物生物量碳、氮含量差异显著。相关性分析表明,除与亚硝酸细菌具有弱正相关性外,海拔高度与其它因子均具有负相关性,其中与细菌和氨化细菌具有极显著负相关性,与好气性固氮菌和硝酸细菌具有显著负相关性。因此,温度的升高可能明显的影响了三江源地区高寒草原的土壤微生物活性。     

不同类型人工湿地微生物群落的研究进展

微生物是人工湿地不可缺少的成员,对湿地生态系统中物质转化、能量流动起着重要作用.本文从人工湿地微生物群落的研究方法、微生物群落结构与组成、微生物群落调节作用与环境因素的关系等方面,综述了人工湿地微生物的研究进展.各种新颖的分子生物学方法已经成为研究人工湿地的微生物多样性的有力工具,其中最常见的是变性梯度凝胶电泳(DGGE)和寡核苷酸荧光探针原位杂交(FISH);人工湿地微生物群落的调节作用主要取决于湿地的水文条件、废水的特点(包括组成成分,污染物的特点和利用性)、湿地的过滤材料或土壤类型、植物和各种环境因素;不同人工湿地类型的微生物群落组成,从多到少依次是变形菌、噬纤维菌.黄杆菌菌群、放线菌和厚壁菌.如何进一步加深对氮循环相关微生物多样性的研究,提高废水中氮的去除效率依然是未来人工湿地技术需要解决的重要问题之一.     

Soil microbial diversity affects soil organic matter decomposition in a silty grassland soil

Soil microorganisms play a pivotal role in soil organic matter (SOM) turn-over and their diversity is discussed as a key to the function of soil ecosystems. However, the extent to which SOM dynamics may be linked to changes in soil microbial diversity remains largely unknown. We characterized SOM degradation along a microbial diversity gradient in a two month incubation experiment under controlled laboratory conditions. A microbial diversity gradient was created by diluting soil suspension of a silty grassland soil. Microcosms containing the same sterilized soil were re-inoculated with one of the created microbial diversities, and were amended with ¹³C labeled wheat in order to assess whether SOM decomposition is linked to soil microbial diversity or not. Structural composition of wheat was assessed by solid-state ¹³C nuclear magnetic resonance, sugar and lignin content was quantified and labeled wheat contribution was determined by ¹³C compound specific analyses. Results showed decreased wheat O-alkyl-C with increasing microbial diversity. Total non-cellulosic sugar-C derived from wheat was not significantly influenced by microbial diversity. Carbon from wheat sugars (arabinose-C and xylose-C), however, was highest when microbial diversity was low, indicating reduced wheat sugar decomposition at low microbial diversity. Xylose-C was significantly correlated with the Shannon diversity index of the bacterial community. Soil lignin-C decreased irrespective of microbial diversity. At low microbial diversity the oxidation state of vanillyl–lignin units was significantly reduced. We conclude that microbial diversity alters bulk chemical structure, the decomposition of plant litter sugars and influences the microbial oxidation of total vanillyl–lignins, thus changing SOM composition.     

Soil microbial community responses to antibiotic-contaminated manure under different soil moisture regimes

Sulfadiazine (SDZ) is an antibiotic frequently administered to livestock, and it alters microbial communities when entering soils with animal manure, but understanding the interactions of these effects to the prevailing climatic regime has eluded researchers. A climatic factor that strongly controls microbial activity is soil moisture. Here, we hypothesized that the effects of SDZ on soil microbial communities will be modulated depending on the soil moisture conditions. To test this hypothesis, we performed a 49-day fully controlled climate chamber pot experiments with soil grown with Dactylis glomerata (L.). Manure-amended pots without or with SDZ contamination were incubated under a dynamic moisture regime (DMR) with repeated drying and rewetting changes of >20 % maximum water holding capacity (WHC_max) in comparison to a control moisture regime (CMR) at an average soil moisture of 38 % WHC_max. We then monitored changes in SDZ concentration as well as in the phenotypic phospholipid fatty acid and genotypic 16S rRNA gene fragment patterns of the microbial community after 7, 20, 27, 34, and 49 days of incubation. The results showed that strongly changing water supply made SDZ accessible to mild extraction in the short term. As a result, and despite rather small SDZ effects on community structures, the PLFA-derived microbial biomass was suppressed in the SDZ-contaminated DMR soils relative to the CMR ones, indicating that dynamic moisture changes accelerate the susceptibility of the soil microbial community to antibiotics.     

Effects of paraquat on selected microbial activities in soil

Paraquat, applied as Gramoxone, to a nonamended sandy loam soil at five times the suggested field application rate (10 lb/A 115g/cm²) increased the numbers of bacteria, actinomycetes, and fungi during a 14-day incubation at 25°C. This increase was attributed to the use of compounds in the Gramoxone formulation rather than the use of paraquat. Treatment at one and five times the normal rate reduced CO₂ evolution by 44% and 67%, respectively, in soil amended with 2% glucose during a 12-day incubation. Similar treatments reduced CO₂ evolution in 1% straw-amended soil by 39% and 58%, respectively, during a 28-day incubation. Cellulose decomposition of cotton duck containing 13 and 176g of paraquat per milligram of material was inhibited for 15 and 28 days, respectively, in soil containing a large population of cellulolytic microorganisms. A concentration of 5000g/gm of paraquat was necessary to inhibit nitrification in soil by 44% druing a 28-day incubation at 20°C. Paraquat inhibited C₂H₂ reduction in artificial aggregates of soil amended with 2% glucose and incubated anaerobically at 25°C. Nitrogenase activity in aggregates was inhibited by 43% and 52% at concentrations of 580 and 720g/gm of paraquat respectively. The inhibitory effects of the herbicide were reduced when soil was amended with organic matter in the form of peat or straw. The availability of paraquat controlled the toxicity of the herbicide to soil microorganisms.     

嫁接对铜胁迫下黄瓜根际土壤微生物特性和酶活性的影响

采用盆栽试验方法,研究了嫁接（以黑籽南瓜为砧木）对铜胁迫下黄瓜根际土壤微生物生物量、微生物种群数量和土壤酶活性的影响.结果表明： 铜胁迫下黄瓜根际土壤微生物生物量碳（MBC）和微生物生物量氮（MBN）含量显著下降,基础呼吸和代谢熵显著上升,但嫁接黄瓜根际土壤MBC和MBN含量显著高于自根黄瓜,而基础呼吸和代谢熵则显著低于自根黄瓜.铜胁迫下,根际土壤放线菌和自生固氮菌的数量显著下降,真菌数量显著上升,而细菌数量变化不显著;嫁接黄瓜根系土壤细菌、放线菌、自生固氮菌的数量显著高于自根黄瓜,而真菌数量显著低于自根黄瓜.嫁接黄瓜根际土壤脲酶、磷酸酶、蔗糖酶、过氧化氢酶活性在铜胁迫下显著高于自根黄瓜.试验结果证明嫁接使铜胁迫下黄瓜根际土壤微生物环境和酶活性得到了改善和提高,从而提高了黄瓜植株对铜胁迫的抵抗力.     

玉米 线辣椒套作系统中土壤养分与根际土壤微生物、酶活性的关系

采用玉米单作、线辣椒单作、玉米-线辣椒套作3种栽培模式,并在玉米-线辣椒套作的种间根部设3种不同隔离处理（膜隔、网隔和无隔）,研究了玉米-线辣椒套作系统中土壤生物因子与土壤养分的关系．结果表明：玉米-线辣椒套作具有明显优势;与两作物单作和玉米-线辣椒套作种间根区膜隔处理相比,玉米-线辣椒根区无隔和网隔处理复合群体中两作物根际土壤酶活性、微生物数量、土壤养分均显著提高;除有效镁与真菌种群数量、过氧化氢酶活性呈负相关外,其余速效养分与各生物因子均呈显著或极显著正相关．通径分析表明,该系统中促进有机质累积的主要生物因素是脲酶、过氧化氢酶、细菌和蛋白酶,蔗糖酶是影响碱解氮的最主要因子,脲酶是影响有效磷的最主要因子,细菌是影响有效钾的最主要因子,碱性磷酸酶、真菌只是选择性地对有机质的累积和氮、磷、钾有效养分的形成起作用,放线菌对土壤养分的直接作用系数为负,对土壤养分形成的作用较小．     

土壤微生物学特性对土壤健康的指示作用

土壤健康是陆地生态系统可持续发展的基础。作者通过概述土壤微生物学特性(土壤微生物群落结构、土壤微生物生物量、土壤酶活性)与土壤质量的关系, 阐明了土壤微生物对土壤健康的生物指示功能。研究表明: 土壤中细菌、真菌和放线菌的组成及其所占比率在一定程度上反映了土壤的肥力水平: 在土壤性质和肥水条件较好的土壤中, 细菌所占比率较高。土壤微生物生物量与土壤有机质含量密切相关, 而且土壤微生物生物量碳与土壤有机碳的比值(C_mic : C_org)和土壤微生物代谢熵(qCO2)的变化在一定程度上反映了土壤有机碳的利用效率。一般情况下, 土壤酶活性高的土壤中, 土壤微生物生物量碳、氮含量也高。因此, 土壤微生物学特性可以反映土壤质量的变化, 并可用作评价土壤健康的生物指标。     

Soil microbial activities and litter decomposition related to altitude

Summary On a southern slope in the Austrian Central Alps (Hohe Tauern Mountains) at altitudes of 2550 m, 1920 m and 1650 m above sea level, respectively, microbial activities were investigated by measuring the decomposition of litter, the cellulase and xylanase activities, CO₂-evolution and the cell counts of viable non differentiated and cellulolytic bacteria. After one year 46% of litter exposed was decomposed at an altitude of 2550 m, 76% at 1920 m and 86% at 1560 m. Investigations with litter bags of different mesh sizes (25 μm and 1000 μm) revealed that small soil animals (<1 mm) did not significantly influence the decomposition of litter at different altitudes and in different vegetation types. The enzymatic activities and the CO₂-evolution of soils decreased with increasing altitude. Plate counts of bacteria from soils at the alpine zone (2550 m) and the tall grass meadow (1650 m) indicated that in some cases the lower metabolic activities caused by bad climatic conditions were compensated by an increase in cell numbers. This work was supported by the Austrian MaB-Hochgebirgsprogramm, Alpine ?kosysteme     

Soil microbial carbon uptake characteristics in relation to soil management

Abstract The kinetics of glucose uptake by soil microbial communities in 16 different soild (7 under monocultures and 9 under crop rotations) differing in microbial biomass content, % C_org, pH and clay content were investigated at 22°C. The V _max value of microbial bimasses under monoculture, was o.27 μg C_gluc · μg⁻¹ C_mic · h⁻¹ (range 0.18–0.44), twice as high as the mean value of V _max of microbial biomasses under rotations (0.13 μg C_gluc, range 0.07–0.19). Mean values of K _m were 714 μg C_gluc and 290 μg C_gluc · g⁻¹ soil, respectively.
These differences were highly significant ( P =0.001, based on SE) and could not be relate to particle size distribution of the soils, pH or C_org. A Michaelis-Menten type uptake response was apparent over the total range of glucose concentrations used (45.4–1453.3 μg C_gluc · g⁻¹ soil) for microbial biomasses under rotation while the majority of microbial biomasses under monocultures showed a similar response only at low glucose concentrations. A different uptake mechanism appeared to be involved at higher glucose concentrations (similar to diffusion) in monoculture soils.     

Soil microbial biomass influence on strontium availability in mine soil

Abstract

The main aim of our work was to assess whether strontium (Sr) affects soil microbial biomass size and activity, and the involvement of said biomass in the availability process of the metal. In addition, information concerning the distribution and mobility of the stable element within ecosystems may allow the prediction of the behaviour of its radioisotope counterpart, ⁹⁰Sr. Samples were collected in the surroundings of a strontium mine and characterised for total and diethylene triamine pentaacetic acid (DTPA)-extractable Sr, total organic C (TOC), microbial biomass C (MBC), MBC/TOC ratio and metabolic quotient (qCO₂). Moreover, MBC and DTPA-extractable Sr were measured during a 45-day incubation experiment of samples soils amended with maize. Overall, increased levels of total Sr had a negative effect on both TOC and MBC. DTPA-extractable Sr was significantly correlated to MBC/TOC suggesting a possible role of soil microbial biomass in the mobilisation of the element. The synthesis of new microbial biomass after soil amendment was negatively affected by the initial content of DTPA-extractable Sr. Conversely, there was a linear positive relationship between newly formed MBC and DTPA-extractable Sr during the incubation, indicating that soil microbial biomass may promote the mobilisation of Sr. These findings indicate that soil amendment with easily degradable organic substrate significantly increases Sr mobility and availability.     

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.     

Effects of mercury on microbial biomass and enzyme activities in soil

Mercury (Hg) is a persistent soil pollutant that affects soil microbial activity. We monitored the changes in soil microbial biomass and activity of enzymes, including alkaline phosphatase, arylsulfatase, fluorescein diacetate (FDA) hydrolytic activity, and o-diphenol oxidase (o-DPO) in three soils contaminated with different concentrations of Hg. Increasing levels of Hg, from 0.5 to 10 μmol/g of dried soil, generally depressed microbial activity; however, the effects of Hg on soil microbial activity depended on soil type and composition, particularly organic matter content. o-DPO was less affected by Hg than the other three enzymes tested. Our results indicate that the analysis of microbial biomass content and soil-enzyme activities may be used to predict the soil quality contaminated with Hg.     

Effects of potassium azide on soil microbial populations and soil enzymatic activities.

Preplant applications of potassium azide (KN3) to pine nursery beds were evaluated for effect on the soil microflora and on soil enzyme activity where either plastic-sealing or water-sealing techniques were used. Two weeks after incorporation of azide (0-224 kg/hs), soil samplings revealed reduced populations of bacteria and fungi and a corresponding decline in invertase and amylase activities. These effects were proportionate to the amount of azide used and were more pronounced in plastic-sealed plots. Phosphatase activity was little affected. Five weeks after azide application, bacterial populations were higher in treated plots than in controls. Greater numbers of bacteria were recorded from plastic-sealed plots and highest populations coincided with plots receiving the highest rates of azide, regardless of the sealing technique. Fungal populations at this sampling were generally less in treated plots than in the controls, but were higher under plastic seal. At this time, changes in invertase and amylase activities did not correspond to increased microbial numbers. Sixteen weeks after applications of KN3, bacterial populations in treated plots did not differ significantly from controls, but remained higher in plastic-sealed than water-sealed plots. Fungal populations under plastic seal had changed little and remained significantly lower in treated water-sealed plots than in controls. The earlier recorded reduction in invertase and amylase activities was still evident at the final sampling;     

红壤茶树根层土壤基础呼吸作用和酶活性

对不同树龄茶树根层土壤的呼吸作用(包括代谢熵qCO2)和土壤酶(脲酶、转化酶和酸性磷酸单酯酶)活性进行了研究、不同树龄茶树根层土壤日基础呼吸作用强度(36．23—58．52mg·kg^-1·d^-1)和日代谢墒(0．30一0．68)都以40和90年茶树较为接近,分别显著大于和小于10年树龄茶树根层土壤;服酶活性(41．48—47、72mg·kg^-1·d^-1)则三者间差异不大,虽然随树龄增长而下降;转化酶活性(189．29—363．40mg·kg^-1·d^-1)也随树龄增长而下降,并且10年茶树根层土壤显著大于40和90年树龄茶树;而酸性磷酸单酯酶活性(444．22—828．32mg·kg^-1·d^-1)相反,随树龄增长而增强．结果表明,土壤基础呼吸作用、代谢熵和3种土壤酶活性都与茶树树龄、土壤pH、土壤有机碳、土壤全氮、土壤可活性酚总量、及土壤微生物生物量密切相关．