松嫩平原苏打盐渍化旱田土壤表观电导率空间变异

在松嫩平原西部吉林省大安市乐胜乡,于2013年4月20日选择盐碱程度不均一的典型盐渍化旱田地块,面积为4.8 hm~2作为研究样地。利用EM38大地电导率仪测定结合田间定点采样,并通过经典统计和地统计相结合的方法研究了盐渍化旱田土壤表观电导率空间变异特征,分析了土壤表观电导率与土壤盐碱指标之间的关系。结果表明,盐渍化旱田土壤水平方向表观电导率(EC_h)经对数转换后具有强空间自相关,其变异特征主要是与地形地貌和水文状况等结构性因素有关。垂直方向表观电导率(EC_v)经对数转换后具有中等空间自相关性,其变异特征受结构性因素和随机因素共同作用。EC_h和EC_v半方差模拟的最优模型分别为球状模型和指数模型。Pearson分析表明土壤表观电导率(EC_h和EC_v)与土壤盐碱指标EC_(1∶5)、pH_(1∶5)、SAR、SC、Na~+、CO_3~(2-)、HCO_3~-呈正相关关系(P0.05),EC_h与土壤盐碱指标相关系数均大于EC_v。在实际应用中可以用EC_h来指示土壤的盐碱程度。回归分析表明土壤表观电导率(EC_h和EC_v)与土壤盐碱指标呈线性相关,且EC_h回归模型的决定系数均大于EC_v回归模型的决定系数,可用水平方向土壤表观电导率(EC_h)来计算土壤盐碱指标,进行土壤盐渍化的快速评估。     

Comparison of five physiological parameters to assess the vitality of the lichen Ramalina lacera exposed to air pollution

To determine the environmental impact of industrial activity, we examined and compared the following parameters of physiological integrity in the epiphytic fruticose lichen Ramalina lacera. (1) Potential quantum yield of PSII expressed as the chlorophyll fluorescence ratio F_v/F_m. (2) Spectral reflectance expressed as values of normalized difference vegetation index (NDVI). (3) Production of ethylene. (4) Electrolyte leakage brought about by degrading cell membranes in terms of electric conductivity. (5) The ratio A_435nm/A_415nm indicating the disintegration of chlorophyll. The amounts of Ba, Cu, K, Ni, S, V and Zn contained in the lichen thallus were measured to quantify the degree of pollution. Some of the lichen‐carrying twigs collected at a relatively unpolluted control site were resuspended on the original trees as controls. Other lichens were transplanted to 19 biomonitoring sites. Transplanted lichens in polluted sites contained higher amounts of Ba, Ni, S, V and Zn than lichens in the control site and in most of the rural sites upon an exposure period of 8 months. Statistical analysis revealed negative correlations between F_v/F_m ratios and Ba contents of transplants. High Ba, Cu, Ni and Zn contents correlated negatively with NDVI values. NDVI values correlated with A_435nm/A_415nm, F_v/F_m and K. The ratio A_435nm/A_415nm correlated positively with K and negatively with Ba, Cu and Zn. The production of ethylene correlated positively with Cu and Ba and negatively with A_435nm/A_415nm, F_v/F_m and NDVI. Electric conductivity values correlated positively with Ba, Cu, Na, S, V and Zn and negatively with NDVI. Both elemental content and physiological alterations in transplants of R. lacera point to a high degree of contamination in the Haifa Bay region, which is polluted by fuel‐oil combustion apart from other industrial activities. The present work suggests that in our specific study area, the most sensitive parameter to assess the vitality of the lichen thallus is electric conductivity whereas ethylene production is less sensitive.     

The annual invasive plant Impatiens glandulifera reduces hyphal biomass of soil fungi in deciduous forests

Soil fungi play a crucial role in ecosystem functioning and there is increasing evidence that exotic plants invading forests can affect soil fungal communities. We examined potential effects of the invasive plant Impatiens glandulifera on hyphal biomass of ectomycorrhizal fungi, their genetic diversity and the diversity of other soil fungi in deciduous forests in Switzerland. We compared invaded patches with patches where I. glandulifera had been removed, by establishing pairs of 3-m long transect lines at the edge of seven areas of either type. Along the transects we assessed the length of ectomycorrhizal fungal hyphae using the ‘ingrowth mesh bag method’, and used terminal restriction fragment length polymorphism (T-RFLP) analysis to examine fungal genetic diversity. The invasive plant reduced fungal hyphal biomass by 30–80%: the reduction was largest in the centre of the patch. I. glandulifera did not alter fungal richness, but affected the composition of fungal communities. This is probably the result of a decrease of mycorrhizal fungi, coupled with an increase of saprotrophic fungi. Our findings demonstrate the adverse impacts of an annual invasive plant species on both fungal hyphal biomass and the composition of soil fungal communities. This may negatively affect forest nutrient and carbon cycling, soil stability and the functionality of the fungal community, with major consequences for forest ecosystem functioning.     

Changes in organic matter composition of forest soil treated with a large amount of urea to promote ammonia fungi and the abilities of these fungi to decompose organic matter

Organic matter composition (lignin, holocellulose, 50% (v/v) methanol extract, water-soluble carbohydrate (WSC) and phenolics (WSP), petroleum ether extract, and ash) of A₀ layer soil treated with 700 g/m² of urea to promote ammonia fungi was investigated in a Japanese red pine (Pinus densiflora) forest. Nine species of fungi were found during the study period of 18 months after the treatment. Of these, seven species belong to the ammonia fungi. WSC content of the treated soil was lower than that of the control. Methanol extract content increased initially after the treatment, then decreased to below the control level. There were no consistent differences in other components between the treated plot and the control. The abilities to decompose cellulose, lignin, chitin, protein and lipid in 18 strains in 10 species of the ammonia fungi were also screened. Cellulose was not lysed byPseudombrophila deerata, Hebeloma spp. andLaccaria bicolor. Strong lignolytic activity was shown byLyophyllum tylicolor, Coprinus echinosporus andP. deerata. Chitin was decomposed byAmblyosporium botrytis, L. tylicolor, C. echinosporus andHebeloma vinosophyllum. All strains possessed proteolytic and lipolytic activities. Supply of glucose to the culture media resulted in weaker enzyme activities except for lignolytic ability.     

Influence of nutrient versus water supply on hydraulic architecture and water balance in Pinus taeda

We investigated the hydraulic consequences of a major decrease in root‐to‐leaf area ratio (A_R:A_L) caused by nutrient amendments to 15‐year‐old Pinus taeda L. stands on sandy soil. In theory, such a reduction in A_R:A_L should compromise the trees’ ability to extract water from drying sand. Under equally high soil moisture, canopy stomatal conductance (G_S) of fertilized trees (F) was 50% that of irrigated/fertilized trees (IF), irrigated trees (I), and untreated control trees (C). As predicted from theory, F trees also decreased their stomatal sensitivity to vapour pressure deficit by 50%. The lower G_S in F was associated with 50% reduction in leaf‐specific hydraulic conductance (K_L) compared with other treatments. The lower K_L in F was in turn a result of a higher leaf area per sapwood area and a lower specific conductivity (conducting efficiency) of the plant and its root xylem. The root xylem of F trees was also 50% more resistant to cavitation than the other treatments. A transport model predicted that the lower A_R:A_L in IF trees resulted in a considerably restricted ability to extract water during drought. However, this deficiency was not exposed because irrigation minimized drought. In contrast, the lower A_R:A_L in F trees caused only a limited restriction in water extraction during drought owing to the more cavitation resistant root xylem in this treatment. In both fertilized treatments, approximate safety margins from predicted hydraulic failure were minimal suggesting increased vulnerability to drought‐induced dieback compared with non‐fertilized trees. However, IF trees are likely to be so affected even under a mild drought if irrigation is withheld.     

Effects of soil water on photosynthetic characteristics and leaf traits of Cyclobalanopsis glauca seedlings growing under nutrient-rich and -poor soil

Cyclobalanopsis glauca is a dominant species in mid-subtropical forest, and usually plays an important role in forest ecosystems. However, it often suffers redundant precipitation or water stress, which often concurs with high temperature, nutrient depletion and strong irradiance. The study presented in the paper hypothesized that soil water exerted strong influence on leaf gas exchange and traits. The objective of this study was to clarify the effect of soil water changes on photosynthetic characteristics and leaf traits and their relationships of C. glauca seedlings growing on nutrient-rich and nutrient-poor soil at three water levels. The study measured the specific leaf area (SLA), nitrogen content, chlorophyll concentrations and photosynthetic light response curve. Its results showed that there were no differences in leaf size, leaf dry weight, SLA, leaf dry matter content, Leaf nitrogen concentration and Leaf chlorophyll between the two soil nutrient treatments, while these parameters differed significantly among different water levels for either of the treatments. There were large variations in leaf photosynthetic parameters and leaf traits among the different water treatments, indicating different response patterns of C. glauca seedling and its adaptation to the different soil water conditions. There were no significant differences in light-saturated photosynthetic rate (A_max) and apparent quantum yield (Ø) between the nutrient-rich and nutrient-poor soils, which indicated that the C. glauca seedlings could maintain similar capacities in different soils that differed in nutrient condition. As to the relation between the photosynthesis and leaf traits, the A_max and PNUE were positively correlated with the SLA, respectively, but the SLA had significant negative relationship with the leaf N (P<0.01) in nutrient-rich soil. In contrast, both A_max and PNUE were significantly negatively correlated with the SLA, respectively (P<0.01); and the SLA was not significantly positively correlated with the leaf nitrogen concentration of the nutrient-poor soil (P>0.05). The specific leaf areas (SLA), nitrogen and chlorophyll concentrations as well as other photosynthetic features were influenced in a coordinative manner by the soil water. The relation among the A_max, PNUE and the N_mass, SLA could be described as a binomial equation and a liner negative regression for the nutrient-rich and nutrient-poor soil, respectively. In conclusion, soil water was more constraining factor than the soil nutrient to the photosynthesis of C. glauca seedlings, nutrient-rich soil could offset some negative influence resulting from soil water deficit on LSP and LCP. Factors affecting the variations of photosynthetic characteristics and leaf traits of C. glauca seedlings differed between the nutrient-rich and nutrient-poor soils.     

Application of terminal restriction fragment length polymorphism (T-RFLP) analysis to monitor effect of biocontrol agents on rhizosphere microbial community of hot pepper (<Emphasis Type="Italic">Capsicum annuum</Emphasis> L.)

Microbial communities in hot pepper (Capsicum annuum L.) cultivation fields under different cultivation methods were investigated by terminal restriction fragment length polymorphism (T-RFLP) analysis. Rhizosphere soil and leaf samples were collected from control, conventional and nature-friendly cultivation fields between May and July, 2009. Two Bacillus subtilis strains were applied to nature-friendly cultivation fields as biocontrol agents during the sampling period. Relative abundances of bacteria and plant pathogenic fungi related T-RFs were also measured to monitor the effect of biocontrol agents on potential plant pathogenic fungi. In the principal component analysis (PCA) based on T-RFLP profiles, the microbial communities from rhizosphere soil samples in July, including bacteria and fungi, showed distinct difference between nature-friendly cultivation fields and other cultivation fields. However, there was no correlation between cultivation methods and leaf microbial communities at any sampling period. Changes in the abundance of bacteria related T-RF in the rhizosphere of nature-friendly cultivation fields were observed clearly two months after application of biocontrol agent, while the abundance of plant pathogenic fungi related T-RFs significantly decreased.     

Ectomycorrhizal exudates and pre-exposure to elevated CO2 affects soil bacterial growth and community structure

Ectomycorrhizal fungi produce low molecular weight organic compounds, supporting diverse microbial communities. To link mycorrhizal root exudation directly to bacterial responses, we used Scots pine exudates with (Suillus variegatus and Piloderma fallax) and without mycorrhiza as substrata for forest soil bacteria. Bacterial growth and vitality was monitored, and community composition determined using T-RFLP, cloning and sequencing. We investigated if the amount of organic acids in exudates explained bacterial growth, and whether bacterial communities were influenced by pre-exposure to elevated atmospheric CO₂. We demonstrated functional differences in bacterial growth rates related to CO₂. There was a shift in the bacterial community (e.g. Burkholderia sp. and gamma-proteobacteria) toward organisms better able to rapidly utilize exudates when pine microcosms were pre-exposed to elevated CO₂. Soil bacteria from all treatments tended to grow more abundantly and rapidly in exudates from Piloderma-colonized seedlings, suggesting that the organic acids and/or unidentified compounds present supported greater growth.     

Carbon quality and soil microbial property control the latitudinal pattern in temperature sensitivity of soil microbial respiration across Chinese forest ecosystems

Understanding the temperature sensitivity (Q₁₀) of soil organic C (SOC) decomposition is critical to quantifying the climate–carbon cycle feedback and predicting the response of ecosystems to climate change. However, the driving factors of the spatial variation in Q₁₀ at a continental scale are fully unidentified. In this study, we conducted a novel incubation experiment with periodically varying temperature based on the mean annual temperature of the soil origin sites. A total of 140 soil samples were collected from 22 sites along a 3,800 km long north–south transect of forests in China, and the Q₁₀ of soil microbial respiration and corresponding environmental variables were measured. Results showed that changes in the Q₁₀ values were nonlinear with latitude, particularly showing low Q₁₀ values in subtropical forests and high Q₁₀ values in temperate forests. The soil C:N ratio was positively related to the Q₁₀ values, and coniferous forest soils with low SOC quality had higher Q₁₀ values than broadleaved forest soils with high SOC quality, which supported the “C quality temperature” hypothesis. Out of the spatial variations in Q₁₀ across all ecosystems, gram‐negative bacteria exhibited the most importance in regulating the variation in Q₁₀ and contributed 25.1%, followed by the C:N ratio (C quality), fungi, and the fungi:bacteria ratio. However, the dominant factors that regulate the regional variations in Q₁₀ differed among the tropical, subtropical, and temperate forest ecosystems. Overall, our findings highlight the importance of C quality and microbial controls over Q₁₀ value in China's forest ecosystems. Meanwhile, C dynamics in temperate forests under a global warming scenario can be robustly predicted through the incorporation of substrate quality and microbial property into models.     

内蒙古草原典型植物对土壤微生物群落的影响

为了分析内蒙古草原不同植物物种对土壤微生物群落的影响, 采用实时荧光定量PCR (real-time PCR)以及末端限制性片段长度多态性分析(terminal restriction fragment length polymorphism, T-RFLP)等分子生物学技术, 测定了退化-恢复样地上几种典型植物的根际土壤和非根际土壤中细菌和真菌的数量及群落结构。结果表明, 不同植物物种对根际和非根际细菌及根际真菌数量均有显著影响。根际土壤中的细菌和真菌数量普遍高于非根际土壤, 尤其以真菌更为明显。对T-RFLP数据进行多响应置换过程(multi-response permutation procedures, MRPP)分析和主成分分析(principal component analysis, PCA), 结果表明, 大多数物种的根际细菌及真菌的群落结构与非根际有明显差异, 并且所有物种的真菌群落可以按根际和非根际明显分为两大类群。此外, 细菌和真菌群落结构在一定程度上存在按物种聚类的现象, 以细菌较为明显。这些结果揭示了不同植物对土壤微生物群落的影响特征, 对理解内蒙古草原地区退化及恢复过程中植被演替引起的土壤性质和功能的变化有一定的帮助。     

重度放牧对欧亚温带草原东缘生态样带土壤氮矿化及其温度敏感性的影响

以欧亚温带草原东缘生态样带为平台,以样带上未放牧和重度放牧配对样地为研究对象,开展重度放牧对欧亚温带典型草原土壤氮矿化及其温度敏感性的影响研究。结果表明:(1)在室内培养条件下,土壤氮积累量和土壤净氮矿化速率呈现出干燥度指数较大的样点显著大于干燥度指数最低的样点(P0.05)。在相对湿润的样点,土壤氮素矿化周转速率较快;(2)重度放牧对不同样点土壤氮积累量和土壤氮矿化速率的影响是不同的。在干燥度指数较高样点,重度放牧样地土壤铵态氮减少量和速率较未放牧样地低(P0.05),重度放牧显著降低了土壤硝态氮积累量、无机氮积累量、硝化速率、净氮矿化速率(P0.05);在干燥度指数较低样点,重度放牧样地土壤铵态氮减少量和速率较未放牧样地高(P0.05),重度放牧对土壤硝态氮积累量、无机氮积累量、硝化速率、净氮矿化速率影响不大(P0.05);(3)土壤氮矿化作用温度敏感性(Q_(10))变化范围在1.61—2.06,重度放牧对Q_(10)无显著影响。随着纬度的升高,Q_(10)呈升高趋势。Q_(10)与基质质量指数以及表观活化能与基质质量指数均呈显著的负相关关系(P0.05);(4)土壤硝态氮积累量、无机氮积累量、硝化速率、净氮矿化速率对重度放牧的响应比与干燥度指数呈极显著负相关(P0.01),重度放牧对欧亚温带典型草原土壤氮矿化的影响受气候条件(温度和降水)的调控。     

Screening of white-rot fungi for their ability to mineralize polycyclic aromatic hydrocarbons in soil

Soil samples from an agricultural field contaminated with 10 ppm¹⁴C-benz(a)anthracene in glass tubes were brought into contact with cultures of wood-rotting fungi, precultivated on wheat straw substrate. Forty-five strains of white-rot fungi and four brown-rot fungi were tested for their ability to colonize the soil and to mineralize¹⁴C-benz(a)anthracene to¹⁴CO₂ within a 20-week incubation time. Twenty-two white-rot fungi and all brown-rot fungi were unable to colonize the soil. Twenty-three strains of white-rot fungi, all belonging to the genusPleurotus, colonized the soil. During the experiment the noncolonizing fungi and their substrate disintegrated more and more to a nonstructured pulp from which water diffused into the soil. The same phenomenon was observed in the control which contained only straw without fungus and contaminated soil. In samples with colonizing fungi the substrate as well as the mycelia in the soil remained visibly unchanged during the entire experiment. Surprisingly, most samples with fungi not colonizing the soil and the control without fungus liberated between 40 and 58 % of the applied radioactivity as¹⁴CO₂ whereas the samples with the colonizing fungi respired only 15–25 % as¹⁴CO₂. This was 3–5 times more¹⁴CO₂ than that liberated from the control (4.9 %) which contained only contaminated soil without straw and fungus. A similar result was obtained with selected colonizing and noncolonizing fungi and soil contaminated with 10 ppm¹⁴C-pyrene. However, in pure culture studies in which¹⁴C-pyrene was added to the straw substrate,Pleurotus sp. (P2), as a representative of the colonizing fungi, mineralized 40.3 % of the added radioactivity to¹⁴CO₂. The noncolonizing fungiDichomitus squalens andFlammulina velutipes liberated only 17.2 or 1.7 %, respectively, as¹⁴CO₂. These results lead to the hypothesis that the native soil microflora stimulated by the formed products of straw lysis is responsible for high degradation rates found with noncolonizing fungi.     

Elevated Atmospheric CO2 Alters Soil Microbial Communities Associated with Trembling Aspen (Populus tremuloides) Roots

Global atmospheric CO₂ levels are expected to double within the next 50 years. To assess the effects of increased atmospheric CO₂ on soil ecosystems, cloned trembling aspen (Populus tremuloides) seedlings were grown individually in 1 m³ open bottom root boxes under either elevated (720 ppm, ELEV) or ambient CO₂ (360 ppm, AMB). After 5 years, soil cores (40 cm depth) were collected from the root boxes and divided into 0–20 cm and 20–40 cm fractions. ELEV treatment resulted in significant decreases in both soil nitrate and total soil nitrogen in both the 0–20 cm and 20–40 cm soil fractions, with a 47% decrease in soil nitrate and a 50% decrease in total soil nitrogen occurring in the 0–20 cm fraction. ELEV treatment did not result in a significant change in the amount of soil microbial biomass. However, analysis of indicator phospholipid fatty acids (PLFA) indicated that ELEV treatment did result in significant increases in PLFA indicators for fungi and Gram-negative bacteria in the 0–20 cm fraction. Terminal restriction fragment length polymorphism (T-RFLP) analysis was used to analyze the composition of the soil bacterial communities (using primers targeting the 16SrRNA gene) and the soil fungal communities (using primers targeting the intergenic transcribed spacer region). T-RFLP analysis revealed shifts in both bacterial and fungal community structure, as well as increases in both bacterial and fungal species richness with ELEV treatment. These results indicated that increased atmospheric CO₂ had significant effects on both soil nutrient availability and the community composition of soil microbes associated with aspen roots.     

基于分数阶微分优化光谱指数的土壤电导率高光谱估算

土壤电导率与含盐量具有高度相关性,精准的土壤电导率监测有助于了解区域土壤的盐渍化程度,对区域盐渍化防治与调控,农业可持续发展以及生态文明建设具有重要意义。为寻求预测土壤电导率的最佳高光谱参数,实现土壤盐分信息的高效监测,本研究对土壤样品进行室内高光谱和电导率测定,利用两波段优化算法对简化光谱指数(nitrogen planar domain index, NPDI)进行波段优化,筛选不同高光谱数据(原始高光谱反射率及其对应的5种数学变换)运算下的最敏感高光谱参数,从而建立土壤电导率高光谱估算模型。结果表明:1)NPDIs与土壤电导率之间的相关性显著,在原数据及其平方根、倒数、对数倒数、1.6阶微分变换形式下,优化光谱指数对土壤电导率的敏感程度更强,相关系数绝对值均超过0.80,且基于1.6阶微分变换的(R_(2020nm)+R_(1893 nm))/R_(1893 nm)波段组合相关系数绝对值最高,达到0.888。2)基于1.6阶微分波段优化的预测模型效果最佳,预测精度为R■=0.84,RMSE_(Pre)=2.07mS/cm,RPD=2.94,AIC=158.11。因此,对高光谱数据的适当数学变换有利于优化光谱指数更好地估算土壤电导率,进一步实现土壤盐渍化高精度动态监测。     

Contrasting effects of extracts from invasive Reynoutria japonica on soil microbial biomass,activity, and community structure

Invasive plants may modify soil properties through the release of phenolic compounds. The effects of phenolics produced by a noxious invader, Reynoutria japonica, on soil microorganisms have rarely been studied in experimental conditions. We performed a laboratory experiment to assess the influence of extracts from R. japonica on soil microbial activity, biomass, and community structure. Two types of extracts (shoots and rhizomes) were added in four concentrations (control—no extract, low—extract diluted 100 times, medium—extract diluted ten times, and high—undiluted extract) to soil collected under native plant species. Concentrations of 12 phenolic compounds, namely catechin, chlorogenic acid, emodin, epicatechin, hyperoside, quercetin, physcion, piceatannol, polydatin, procyanidin B3, resveratrol, and resveratroloside were analyzed in the extract and soil. We measured the activity of five enzymes, namely acid and alkaline phosphatases, β-glucosidase, phenoloxidase, peroxidase, the activity of bacteria on Biolog Ecoplates, as well as the biomass of bacteria, saprotrophic fungi, arbuscular mycorrhizal fungi (AMF), and microbial community structure using phospholipid (PLFA) and neutral (NLFA) fatty acid analysis. Many microbial parameters, namely phosphatase activities, total microbial, AMF, and G?+?bacterial biomass, were reduced following the addition of extracts. This was likely related to phenolics as concentrations of these compounds in soil increased with the concentration of extract added. In contrast, saprotrophic fungi and G- bacteria were largely positively affected by extract addition. Shoot and rhizome extracts had relatively similar effects on the soil properties. The changes in soil biota caused by R. japonica invasion may have implications for restoration of invaded areas.

     

重庆酸雨区不同林型对土壤酸化和真菌群落的影响

不同林型土壤的酸化缓冲能力不同,真菌在土壤系统中扮演着重要的角色,而对土壤真菌群落结构和组成与土壤酸化的关系缺乏深入研究。以重庆铁山坪林场的马尾松纯林（Pi）和经马尾松纯林改造后的香樟纯林（Ci）、木荷纯林（Sc）、马尾松-香樟混交林（Pi_Ci）以及马尾松-木荷混交林（Pi_Sc）为研究对象,每个林型分别设置4个20 m×20 m的样地,分别采集腐殖质层（O层）和淋溶层（A层）土壤进行土壤性质及真菌群落分析,以探讨酸雨区森林土壤真菌群落与缓解土壤酸化的关系。研究表明：（1）与Pi相比,Ci土壤酸化明显缓解（高pH低NH₄ ： NO₃）,且能有效提高土壤全磷（TP）含量;而Sc虽然土壤pH值与Pi没有显著差异,但显著（P<0.05）提高了NH₄ ： NO₃,且显著降低土壤TP和全钾（TK）含量（P<0.05）;（2）不同林型土壤真菌群落多样性以Ci最为丰富,且表征土壤酸化的指标pH值、阳离子交换量（CEC）与真菌多样性显著正相关（P<0.05）,NH₄ ： NO₃与多样性显著负相关（P<0.05）;（3）林型和土层都对真菌群落结构有显著影响（P<0.001）,且林型的影响大于土层的影响;而土壤酸化程度将五个林型的土壤真菌群落区分成两个大类：Ci和Pi_Ci;Pi,Sc以及Pi_Sc。（4） Ci中有益菌（如Mortierella）更多,Pi以外生菌根真菌占优势（Russulaceae、Russula、Tomentella以及Sebacina）;Sc以及Pi_Sc则含有更多的植物病原菌（Cladophialophora,Paecilomyces,Venturiales）、嗜酸菌及产酸菌（Paecilomyces,Penicillium）。在酸雨区受损马尾松林地种植香樟促进土壤真菌多样性提高,且产酸真菌、嗜酸菌丰度降低,而有益真菌丰度增加,可有效缓解土壤酸化;而种植木荷后土壤中的病原菌、嗜酸菌和产酸菌相对丰度增加,导致土壤进一步酸化。因此,通过将受酸雨损害严重的马尾松纯林改造成香樟纯林或马尾松-香樟混交林,有助于缓解土壤的酸化,实现酸雨区森林生态系统的可持续发展。     

Role of eukaryotic microbiota in soil survival and catabolic performance of the 2,4-D herbicide degrading bacteria <Emphasis Type="Italic">Cupriavidus necator</Emphasis> JMP134

Cupriavidus necator (formerly Ralstonia eutropha) JMP134, harbouring the catabolic plasmid pJP4, is the best-studied 2,4-dichlorophenoxyacetic acid (2,4-D) herbicide degrading bacterium. A study of the survival and catabolic performance of strain JMP134 in agricultural soil microcosms exposed to high levels of 2,4-D was carried out. When C. necator JMP134 was introduced into soil microcosms, the rate of 2,4-D removal increased only slightly. This correlated with the poor survival of the strain, as judged by 16S rRNA gene terminal restriction fragment length polymorphism (T-RFLP) profiles, and the semi-quantitative detection of the pJP4-borne tfdA gene sequence, encoding the first step in 2,4-D degradation. After 3 days of incubation in irradiated soil microcosms, the survival of strain JMP134 dramatically improved and the herbicide was completely removed. The introduction of strain JMP134 into native soil microcosms did not produce detectable changes in the structure of the bacterial community, as judged by 16S rRNA gene T-RFLP profiles, but provoked a transient increase of signals putatively corresponding to protozoa, as indicated by 18S rRNA gene T-RFLP profiling. Accordingly, a ciliate able to feed on C.␣necator JMP134 could be isolated after soil enrichment. In␣native soil microcosms, C. necator JMP134 survived better than Escherichia coli DH5α (pJP4) and similarly to Pseudomonas putida KT2442 (pJP4), indicating that species specific factors control the survival of strains harbouring pJP4. The addition of cycloheximide to soil microcosms strongly improved survival of these three strains, indicating that the eukaryotic microbiota has a strong negative effect in bioaugmentation with catabolic bacteria.     

Colonization capacity of the soil micro-organisms in relation to fungistasis

Summary Evans' tube and cellophane agar-disc techniques were used to evaluate the colonization capacity of the soil microbes and fungistasis, respectively. Spore germination ofAlternaria tenuis, Curvularia geniculata, Helminthosporium rostratum andPestalotia sp. was studied on a natural soil. Aspergillus fumigatus was the pioneer colonizer, followed in the order of decreasing colonizing capacity by,A. flavus, A. niger, A. terreus andPenicillium nigricans. Sensitivity of test spores to soil fungistasis declined in the order,C. geniculata → Pestalotia sp. →A. tenuis → H. rostratum. The fungistatic level of the soil samples decreased gradually from side arms 1 to 7 of the Evans tube, inoculated with unsterilized soil from one end. Studies conducted with an inoculum of four soil fungi (A. fumigatus, A. flavus, A. niger, andP. nigricans) as well as those involving fumigation of Evans tube by CS₂ also proved the greater colonizing capacity ofA. fumigatus. The level of fungistasis followed closely the colonization pattern of this fungus. When added individually to the soil, all fungi were able to inhibit spore germination of test fungi to some degree or other.     

煤矿复垦区土壤水动力学特性对下渗过程的影响

煤矿复垦区土壤水对植物生长、溶质运移以及土壤环境的变化起着至关重要的作用。定量揭示煤矿复垦区土壤水下渗过程是亟待诠释的关键科学问题。本研究通过测定典型矿区不同深度土壤非饱和导水率、容重、总孔隙度和粒径等水动力学参数,结合染色示踪试验,刻画矿区非饱和带土壤水运移过程。染色示踪结果显示30、60 L和90 L这3种实验下渗水量条件下,水流沿X方向侧向扩散的最大距离分别为10、30 cm和35 cm,沿Y方向侧向扩散的最大距离分别为10、25 cm和30 cm。互相关函数显示随着下渗水量增大,水流扩散作用也在加强,但过多水量并没有明显增加下渗深度和扩散距离。吸力大于300 hpa时,0.01—0.05 mm土壤粒径含量和非饱和导水率呈负相关关系;吸力和非饱和导水率采用指数函数拟合效果较好(r~20.9),对拟合参数a、b和土壤容重(x)进行回归分析:a=0.0015x~2-0.00499x+0.0004,b=0.0583x~2+0.1234x-0.072。同一吸力下土壤容重大的土样非饱和导水率较小;吸力值为300 hpa是非饱和导水率的转折点;非饱和导水率和土壤容重呈现负相关关系,和总孔隙度呈现正相关关系,且二者的相关性随吸力的增加而降低。     

Rice roots select for type I methanotrophs in rice field soil

Methanotrophs are an important regulator for reducing methane (CH₄) emissions from rice field soils. The type I group of the proteobacterial methanotrophs are generally favored at low CH₄ concentration and high O₂ availability, while the type II group lives better under high CH₄ and limiting O₂ conditions. Such physiological differences are possibly reflected in their ecological preferences. In the present study, methanotrophic compositions were compared between rice-planted soil and non-planted soil and between the rhizosphere and rice roots by using terminal restriction fragment length polymorphism (T-RFLP) analysis of particulate methane monooxygenase (pmoA) genes. In addition, the effects of rice variety and nitrogen fertilizer were evaluated. The results showed that the terminal restriction fragments (T-RFs), which were characteristic for type I methanotrophs, substantially increased in the rhizosphere and on the roots compared with non-planted soils. Furthermore, the relative abundances of the type I methanotroph T-RFs were greater on roots than in the rhizosphere. Of type I methanotrophs, the 79 bp T-RF, which was characteristic for an unknown group or Methylococcus/Methylocaldum, markedly increased in field samples, while the 437 bp, which possibly represented Methylomonas, dominated in microcosm samples. These results suggested that type I methanotrophs were enriched or selected for by rice roots compared to type II methanotrophs. However, the members of type I methanotrophs are dynamic and sensitive to environmental change. Rice planting appeared to increase the copy number of pmoA genes relative to the non-planted soils. However, neither the rice variety nor the N fertilizer significantly influenced the dynamics of the methanotrophic community.