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1.
藏中矿区重金属污染土壤的微生物活性变化   总被引:11,自引:0,他引:11  
微生物几乎参与土壤中的一切生物及生物化学反应,土壤微生物活性可较敏感地反映土壤中生化反应的方向和强度,是探讨重金属污染生态效应的有效途径之一。通过野外调查与采样和室内分析,研究了藏中矿区重金属污染对土壤酶活性、基础呼吸、代谢商(qCO2)和可矿化N的影响。结果表明,矿区土壤受重金属Cu、Zn、Pb、Cd不同程度污染,使得土壤酶活性、可矿化N受到抑制,基础呼吸和qCO2则受到刺激。逐步多元回归分析表明,在Cu、Zn、Pb、Cd复合污染条件下,矿区土壤重金属复合污染对土壤微生物活性的影响是复杂的;主成分分析表明,土壤总体微生物活性指标能较好地反映拉屋矿区土壤重金属复合污染状况,可作为藏中矿区土壤环境质量评价及量化分类的有效指标。  相似文献   

2.
There is currently a wide variety of methods used to evaluate soil contamination. We present a discussion of the advantages and limitations of different soil contamination assessment methods. In this study, we analyzed seven trace elements (As, Cd, Cr, Cu, Hg, Pb, and Zn) that are indicators of soil contamination in Dexing, a city in China that is famous for its vast nonferrous mineral resources in China, using enrichment factor (EF), geoaccumulation index (Igeo), pollution index (PI), and principal component analysis (PCA). The three contamination indices and PCA were then mapped to understand the status and trends of soil contamination in this region. The entire study area is strongly enriched in Cd, Cu, Pb, and Zn, especially in areas near mine sites. As and Hg were also present in high concentrations in urban areas. Results indicated that Cr in this area originated from both anthropogenic and natural sources. PCA combined with Geographic Information System (GIS) was successfully used to discriminate between natural and anthropogenic trace metals.  相似文献   

3.
Modern mining technologies promote the nation's gross domestic product and reduce environmental impacts; however, previous mining activities in Missouri have a legacy of soil contamination. This study focuses on Pb-Cd-Zn-Ag-In soil contamination resulting from a closed Pb-Zn mine at St. Joe State Park in Missouri. Metal contamination is the result of ancestral smelting operations and presently exposed tailings. Three soil profiles located adjacent to a closed mine-smelting operation and two reference pedons located outside of the study area were examined to determine the concentrations of Pb, Cd, Zn, Ag, and In. Aqua regia digestion and selective chemical extractions were employed to assess metal availability. The near-surface soil horizons show dramatically greater Pb, Cd, Zn, Ag, and In concentrations than deeper soil horizons or the reference loess-derived soil profiles. Surface Pb concentrations in the study area range from 224 to 589 mg Pb kg ? 1 , whereas the surface Cd concentrations range from 0.3 to 3.1 mg Cd kg? 1. Pyrophosphate and EDTA (Ethylenediaminetetraacetic Acid) extractions demonstrate that a small to substantial portion of the total Pb and Cd pool is potentially available. Water soluble metal concentrations infer that the risk of metal leaching from the soil is minimal.  相似文献   

4.
Toxic metal contamination in the vicinity of Korean abandoned metal mines has been reported. A risk assessment for these metals was performed for the inhabitants in the area of the abandoned Jukjeon metal mine. Soil, groundwater, and crop samples were collected around the mine. After pretreatment of these samples, metal concentrations were measured and then a risk assessment was performed using the Korean soil-contamination risk assessment guidelines. Phytoaccumulation of metals in crops was observed in soybeans (As and Zn), red peppers (Zn), sweet potatoes (As and Zn), and cabbage (Cu), which had higher metal concentrations than soils in the area. The metal intake rate was highest for inhalation of soil. Cancer risk was highest from ingestion of As-contaminated crops. The sum of carcinogenic risks was 6.29 × 10–3. The non-carcinogenic risk was highest for ingestion of As-contaminated crops (8.17). Most of the risks were attributable to As, Pb, and Hg contamination, therefore these three metals must be considered as the principal metals toxic to human health in the sampled area. In particular, the inhalation of metal-contaminated soil should be considered for risk assessment along with ingestion of water and crops in abandoned mine areas.  相似文献   

5.
Abstract

Tungsten (W) mining has taken place in Ganzhou in China for about 100 years. Such long-term W mining may release large amount of metals to soils and waters around these mines. Twenty soil samples were taken from the area around the W mines and 10 soil samples from an area much farther away. These soil samples were analysed for physicochemical properties, heavy metal content and their chemical forms. Results show that long-term W mining significantly increased both total and labile contents of Cd, Cu, Pb and Zn, but did not, or only slightly, increased the total content of Co, Cr and Ni in the soil near the mine. Average enrichment factor (EF) in the agricultural soils was 4.0, 2.4, 2.2, and 2.0 for Cd, Cu, Pb and Zn, respectively. The labile fraction was dominated by the carbonate-bound fraction for Cd (54.5%) and organic matter-bound fraction for Cu (37.9%), while the major labile fractions for Pb and Zn were associated with carbonates (30.2% and 6.4%), oxides (17.9% and 10.6%) and organic matter (9.2% and 18.8%). Consequently, there is a need to be cautious about Cd in the soils contaminated by W mining.  相似文献   

6.
Abstract

A preliminary study on soil contamination with heavy metals and As based on solid phase speciation according to the Tessier scheme and the influence on groundwater in an area under anthropogenic influence (Bozanta-Baia Mare, Romania) was conducted. The partitioning of Al, As, Cd, Cu, Fe, Mn, Pb and Zn in five fractions is discussed in relation to soil characteristics, pH, organic matter content, mineralogical composition and distribution of the same elements in airborne particulate matter. The airborne particulate matter contains high quantities of As, Cd, Cu, Pb and Zn as exchangeable fraction. The sequential extraction carried out on soil samples revealed the main role of Fe-Mn oxides surface in the immobilization of metals. Organic matter has a specific role in complexation of Cu, Pb, As and Al, since high contents of these metals were recovered in the oxidizable fraction. Cadmium has a high selectivity for carbonate minerals. The amendment of soil with natural fertilizer increases the exchangeable fraction of metals with the highest toxicity. The available fraction for plants (exchangeable + carbonate-bound species) exceeded the alert values in soil, therefore the continuous monitoring of the area is necessary. The soil is unsuitable for agricultural use due to high contamination on surface with toxic elements resulted from anthropogenic activities. Groundwater is contaminated with very toxic elements (As, Cd and Pb) but also with Cu, Mn and Zn and is unsuitable as supply for drinking water.  相似文献   

7.
五节芒对重金属污染土壤微生物生物量和呼吸的影响   总被引:6,自引:0,他引:6  
选择3个五节芒在重金属污染地的定居点作为研究样地,其中两个为Pb/Zn矿尾矿砂堆积地(W:黄岩铅锌尾矿;Y:三门铅锌尾矿),一个为冶炼厂附近污染农田(N),分别测定其根围与根际土壤微生物基础呼吸、微生物量碳、微生物量氮、土壤理化特性和土壤重金属含量.结果表明:根际土壤微生物基础呼吸和微生物量氮均显著地高于根围土壤(P<0.05),除了N样地外,微生物量碳在根围与根际之间差异不显著(P>0.05).根际土壤有机碳、总氮(Y样地除外)和离子交换量(N样地除外)低于根围土壤.根际重金属(Pb、Zn、Cu、Cd)总量与DTPA(二乙三胺五乙酸)可提取量普遍低于根围土壤.冗余分析(RDA)表明,根围和根际土壤微生物与土壤理化特性呈不同程度的正相关,而与土壤重金属含量呈现不同程度的负相关.主分量及回归分析同样证明土壤微生物总体变化与土壤理化特性呈正相关(根围R2=0.653;根际R2=0.690),而与重金属含量呈负相关(根围R2=0.610;根际R2=0.662).  相似文献   

8.
不同土壤生境下斑茅对重金属的富集特征   总被引:1,自引:0,他引:1  
为了筛选Cu、Zn、Pb、Cd多重金属离子的富集植物,对不同土壤生境(铜铁矿、钨矿、铅锌矿和无矿场污染)的优势种斑茅(Saccharum arundinaceum(Retz.)Jeswiet)对Cu、Zn、Pb、Cd离子富集情况进行了调查。结果表明,斑茅对Cu、Zn、Pb、Cd离子有富集优势并以Cu富集显著,斑茅根系土壤与斑茅地上部Cu含量存在相关性(P<0.05),斑茅对Pb和Cd的富集与转运存在极显相关性(P<0.01);在强酸、多金属污染弃耕农田土壤中,斑茅不仅符合Cu超富集植物的特征,而且其对Zn、Pb和Cd3种重金属的富集系数和转运系数均>1。在Cd、Cu、Pb和Zn均低于国家土壤环境质量二级标准(GB15618-1995)的弃耕农田中,斑茅对Cu、Zn和Cd的富集系数均>1。研究表明,斑茅可以作为Cu、Zn、Pb、Cd多金属污染土壤的富集植物进行人工修复。  相似文献   

9.
The high-sulfur containing coalmine overburden (OB) dumping ground of the Tirap colliery under the northeastern coalfields in Assam, India, was reclaimed by phytoremediation techniques. Native plant species were planted with line and field methods and by amending with cow dung and unmined soil. In this study, the changes in microbial activity of the reclaimed mine OB wasteland of the Tirap colliery are examined. The enzyme activities of urease, dehydrogenase, and phosphatase were compared over time. Improvements in soil pH, bulk density, and water-holding capacity in the mine OB were found. After four years of reclamation, 1.01% of particles were soil sized (=0.255 mm grain size) with the maximum degradation in the mine OB grain sizes of ?20 mm to +12 mm and of +25 mm. A 1,000-fold increase in microbial colony forming units (CFU) in the four years at the remediated site along with an increase in total DNA were evident for the mine OB reclaimed sites. The increase of microbial CFUs in the mine OB was related to a 100- to 2,000-fold increase in enzyme activity for the reclaimed areas. From this investigation, it can be concluded that the improvement of enzyme activities and the increase in microbial populations of reclaimed mine OB will yield information pertaining to the reclamation index of mine OB.  相似文献   

10.
砷矿区农田土壤微生物群落碳源代谢多样性   总被引:4,自引:0,他引:4  
采用Biolog方法研究了砷(As)矿区农田土壤微生物碳源利用多样性及其与土壤化学性质的关系.结果表明: 3种土壤的N、P、K、有机质(OM)、Cu和Zn全量依次为中As > 高As > 低As土壤.中As和高As土壤微生物平均吸光度以及多样性指数(H′、D、U)显著高于低As土壤.主成分分析与生理碳代谢指纹图谱分析表明,中As和高As土壤微生物对糖类、氨基酸类等碳源的利用程度显著高于低As土壤.典范对应分析显示,影响土壤微生物群落碳源代谢的主要有全P、OM、全Pb、全Zn、全N和pH,全As并不是最主要的影响因子.可见,养分是影响长期污染土壤微生物群落结构和功能多样性的主要因素.  相似文献   

11.
Many mine spoils present at the surface of reclamation sites in the Lower Lusatian mining district are carboniferous substrates, i.e. contain geogenic organic matter. Depending on its susceptibility to microbial degradation, geogenic organic matter might influence the establishment of a carbon requiring microflora in mine spoils. As geogenic organic matter contains substantial amounts of organic nitrogen it is also a potential source for plant available N. The objective of the present study was to quantify C and N mineralisation and microbial biomass in geogenic organic matter present at reclamation sites in Lower Lusatia. We also studied, whether these properties can be influenced by raising the originally low pH to near neutral conditions. In laboratory incubation studies, the rates of CO2 evolution and net N mineralisation were determined in geogenic organic matter and carboniferous mine spoil with and without addition of lime. At the same time, microbial biomass carbon was estimated. As a reference, soil organic matter originating from the humus layer of a 60-year-old Pinus sylvestris stand was used. As indicated by the initial rates of C mineralisation, geogenic carbon was microbially available but to a lower extent than soil organic carbon. During incubation, C mineralisation remained constant or tended to increase with time, depending on the origin of the sample, while it decreased in soil organic matter. Unlike in soil organic matter, in geogenic organic matter and carboniferous mine spoil, C mineralisation was not consistently promoted by lime addition. Prior to incubation, microbial biomass in geogenic organic matter and carboniferous mine spoil was about 10-fold lower than in soil organic matter and tended to increase with incubation time while it decreased in soil organic matter. Similar to C mineralisation, microbial biomass in geogenic organic matter increased after liming, while it declined in carboniferous mine spoil immediately after lime addition. Rates of net N mineralisation were very low in geogenic organic matter and carboniferous mine spoil regardless of the length of incubation and could not be enhanced by raising the pH. It was concluded, that in mine spoils where accumulation of soil organic matter has not yet occurred, geogenic organic matter can be favourable for the establishment of a heterotrophic microflora. However, in the short term, geogenic matter is no source for plant available N in mine spoils. This revised version was published online in June 2006 with corrections to the Cover Date. This revised version was published online in June 2006 with corrections to the Cover Date. This revised version was published online in June 2006 with corrections to the Cover Date.  相似文献   

12.
研究了陕西省铜川煤矿矿区的重金属污染状况以及不同程度的重金属污染对土壤微生物代谢、微生物群落功能以及土壤酶活性的影响.结果表明: 铜川矿区土壤中重金属Cu、Zn、Cd、Pb全量及有效量均显著高于非矿区土壤,其中Cd污染最为严重.采用Biolog方法结合主成分分析和聚类分析发现,随着污染程度的增加,不同土壤微生物群落间的代谢特征发生显著变化,而且这种变化主要体现在糖类和氨基酸类碳源的利用差异.在轻度、中度污染情况下,土壤微生物群落对碳源的利用表现出激活效应;而在重度污染的情况下,土壤微生物群落对碳源的利用表现出抑制效应.随着污染程度的增加,脲酶、蛋白酶、碱性磷酸酶和过氧化氢酶的活性均呈现降低的趋势,矿区土壤脲酶、蛋白酶、碱性磷酸酶和过氧化氢酶活性分别是非矿区土壤中相应酶活性的50.5%~65.1%、19.1%~57.1%、87.2%~97.5%、77.3%~86.0%;蔗糖酶和纤维素酶在中等污染程度以下的土壤中表现为激活效应,而在重度污染的土壤中表现为抑制效应.  相似文献   

13.
The spatial and vertical distributions of heavy metals were quantitatively determined for organic-rich agricultural soils in the Southwestern Nile Delta. This study aims to undertake an assessment of heavy metals contamination in the soils of Quessna district using the inductively coupled plasma-optical emission spectroscopy, remote sensing, and geographic information system techniques. In this study, 24 soil samples were collected at 12 sites representing the main suburbs in the Quessna district. The concentrations of the studied metals decreased in the order of Zn > Cr > Pb > Cu > Ni > Co. The contamination degree and ecological risk assessment for metals in soil samples were evaluated using the enrichment factor, geoaccumulation index, improved Nemerow's pollution index, Pollution load index, and potential ecological risk index. The spatial and vertical distribution of heavy metals concentrations were affected by soil properties such as clay and organic matter content and scavenger metals (Fe and Mn). The intensive urbanization, industrial activity, and agricultural practices are thought to be the main anthropogenic sources of heavy metals contamination. Further studies especially human health risk assessment are recommended to investigate possible risks for humans from heavy metals in this area.  相似文献   

14.
This study investigated the concentrations of Co, Cr, Cu, Mn, Ni, Pb and Zn in surface soil and corn cob samples collected from agricultural fields near a coal mine from Huaibei, China. Meanwhile, the mobility and availability of heavy metals in soil samples were evaluated by a modified three-step The European Community Bureau of Reference (BCR) sequential extraction procedure. The total concentrations of metals in soil pose no ecological threats to the local plants. Transfer factors of essential metals, Cu and Zn, as well as those of non-essential metal Pb, were higher than those of the remained metals. The results of BCR fractionation analysis revealed that the acid soluble, reducible and oxidizable fractions of the Mn, Pb and Zn were higher than those of the residual fraction, suggesting that these elements may be more bioavailable. The pH and organic matter contents of soil were significant parameters affecting speciation of metals in soil samples. Hierarchical cluster analysis indicated significant correlations between metal levels in corn grains and more available (acid soluble and reducible) fractions in soil, indicating that heavy metals in the first two fractions were more available for corn crops. The elevated mobility and bioavailability of Pb in soil are of great concern in the study area.  相似文献   

15.
A great number of potentially toxic elements are introduced into soils by numerous anthropogenic activities, such as the foundry industry and may have negative consequences on the environment and subsequently on human health. This paper reports the characterization of soil samples collected at the facilities of an old foundry, already demolished, that operated during the last century in an industrial area in the Center of Portugal, Coimbra. The mineralogy, physicochemical parameters, and geochemistry of the soil foundry's area, were studied and compared with regional soil parameters to understand the impact of the foundry's activity on the soil. The enrichment and degree of contamination in the factory soil were also assessed, according to public guidelines. Foundry soil was found to exhibit higher average contents of Al2O3, Fe2O3(t), SiO2, TiO2, Zr, Sr, Rb, Pb, Zn, Cu, V, Nb, and Bi, than the corresponding regional baseline values. Specifically, the soil in the foundry area is polluted with Cu, Pb, and Zn. PCA analysis allowed to distinguish the natural soil from the foundry contaminated soil and the contribution of the spent sands and iron slags in the modification of the geochemistry of the regional soil. The contaminants and pollutants are not uniformly distributed as they show the higher concentrations in places of local storage, disposal, and finishing of materials used in the foundry.  相似文献   

16.
对湖南省石门、冷水江、浏阳3个矿区土壤和苎麻体内重金属进行测定和分析。结果表明,石门雄黄矿区As污染严重,伴随Cd、Sb污染和轻微的Pb污染;冷水江锑矿区Sb为主要污染物,伴随Cd、As、Pb污染;浏阳七宝山矿区Cd污染严重,伴随Pb、Zn、Cu污染。15个采样点的苎麻群落生长繁茂,Sb和As在苎麻不同部位间的分布次序为叶片中含量最高,根茎中次之,其余重金属在部位间分布没有规律。所有采样点苎麻地上部的Cd含量比一般植物的Cd含量大2-10倍,As含量大9.9-147.5倍,Sb含量大1.2-338.4倍;Cd富集系数和转移系数最高值为2.07和3;As富集系数和转移系数最高值为1.04和12.42,Sb富集系数和转移系数最高值为1.91和9.04。3个矿区苎麻地上部生物量分别为3.47,14.3,15.7 t/hm2,地上部Cd、Pb、As、Sb、Zn和Cu的累积量分别高达0.11、1.17、0.72、7.97、6.71,1.69 kg/hm2,兼具一定的经济价值和观赏性,适合用作矿区重金属污染土壤的环境治理和修复。  相似文献   

17.
德兴铜矿尾矿重金属污染对土壤中微生物多样性的影响   总被引:12,自引:2,他引:10  
【目的】为更好地了解重金属污染与微生物多样性之间的相互作用关系,以江西德兴铜矿4#尾砂库为研究对象,采集野外实地样品共16件进行分析(包括尾砂样品以及周围农田和菜地土壤样品)。【方法】一方面对样品中可培养异养细菌进行平板计数,一方面采用变性梯度凝胶电泳(Denaturing gradient gel electrophoresis,DGGE)对样品中可培养和不可培养微生物分子生态多样性进行研究;同时采用PCA(Principle component analysis)方法分析样品理化性质、重金属及主要元素与可培养细菌数量及微生物多样性之间的相互关系。【结果】元素分析结果表明该尾矿区样品受到不同程度重金属Cu、Cd、Zn、Ni、Pb和Cr的污染;可培养异养细菌在尾砂样品中数量最少,在菜地和农田土壤样品中有明显增加;多样性指数(Shannon-Weaver index H)计算结果发现H最大值出现在距离尾矿中等距离、重金属浓度在中等程度的样品中。PCA分析结果表明可培养异养菌数量与理化性质如有机碳、有机质、含水率等相关性较大,重金属影响不明显;而多样性指数H除与上述理化性质相关性较大外,还受到重金属Ag、Zn、As、Pb、Ni、Cr等的影响,而在样品中含量普遍比较高的重金属如Cu、Cd等并不成为影响微生物多样性的主要因素。【结论】从这些长期受重金属污染的野外实地样品来看,以上结果说明不同重金属浓度对微生物多样性的影响可能并不是实验室研究的简单的线性关系。  相似文献   

18.
种植香根草对铜尾矿废弃地基质化学和生物学性质的影响   总被引:6,自引:0,他引:6  
徐德聪  詹婧  陈政  高毅  谢贤政  孙庆业  豆长明 《生态学报》2012,32(18):5683-5691
通过实地调查取样和室内分析,研究铜陵水木冲铜尾矿废弃地不同时期种植香根草(Vetiveria zizanioides L.)群落(近期种植香根草群落(V.zizanioides communities were established in the recent stage,JX),中期种植香根草群落(V.zizanioides communities were established in the middle stage,ZX)和早期种植香根草群落(V.zizanioides communities were established in the early stage,OX))对尾矿基质化学性质、微生物量和土壤酶活性的影响,探讨人工植被恢复对铜尾矿废弃地基质系统的修复作用。结果表明:香根草的定植能延缓铜尾矿的酸化过程,且随着香根草定植时间的延长,0—5 cm和5—20 cm层尾矿基质中总氮和速效磷含量提高(其中,0—5 cm层总氮积累更加显著),OX下0—5 cm表层基质总氮和速效磷的平均值分别是JX下的4.64倍和22.44倍。基质微生物量C、N含量和脱氢酶、过氧化氢酶、脲酶活性也随香根草种植时间的延长而有不同程度的升高,且基质化学性质对微生物量和酶活性有影响,其中基质微生物量C、N含量、脱氢酶和过氧化氢酶活性均与电导率呈显著或极显著负相关性;而基质微生物量N和4种酶活性均与总氮含量呈显著或极显著正相关性,表明总氮含量是影响基质微生物量N和酶活性的主要因子;基质微生物量N、脱氢酶和过氧化氢酶活性还与速效磷含量呈极显著正相关性。基质中Cu、Pb含量对脱氢酶、过氧化氢酶活性和微生物量均有显著抑制作用,而Zn对基质微生物活性有一定的激活作用。生长在尾矿废弃地上的香根草不仅显著地改善了铜尾矿废弃地的基质化学性质,且有利于基质微生物量和酶活性的增加,是一种良好的矿业废弃地生态修复物种。  相似文献   

19.
Abstract

The spatial distribution of six heavy metals (Cd, As, Zn, Pb, Cr, and Cu) in the soil of a decommissioned uranium mining area was investigated and their potential environmental risk was assessed. Soil samples were collected along the main riversides enclosing the mining area. The heavy metal distribution was determined by geospatial interpolation. Pearson correlation coefficient and principal component analysis were used to locate the sources of pollution which are the mine ore as natural source, and dressing plants and tailing area from human activity. The results indicate that the average concentrations of As and Cd strongly exceed the recommended EQSS (Environmental Quality Standard for Soils of China) limits at all sampling sites, whereas Zn concentrations were found to be slightly over the limit only at sampling sites close to the mining area. The concentrations of Cr, Cu and Pb were all within the recommended limits. Environmental risk was assessed using the toxicity characteristic leaching procedure defining the degree to which extend the metal is released into the solution. High leaching rates were found only for Zn and Cd, suggesting that together with its high concentrations Cd is the most toxic metal around the mining area, followed by As.  相似文献   

20.
随着全球氮沉降速率的快速增加,已对陆地生态系统微生物群落活性和代谢产生了深刻的影响。因此迫切需要了解全球气候变化敏感区土壤中微生物量和酶活性对氮添加的响应。为此,以中亚干旱区巴音布鲁克高寒湿地为研究对象,在保护良好的高寒湿地选择沼泽(S)、沼泽草甸(SM)和草甸(M)3种湿地类型布设野外原位氮添加试验(施氮浓度分别为0、8、16 kg N hm-2 a-1),探究短期氮添加对土壤微生物生物量碳(MBC)、微生物生物量氮(MBN)、微生物生物量碳/氮(MBC/MBN)、微生物商(QMB)、土壤蛋白酶、脲酶、碱性磷酸酶、H2O2酶和蔗糖酶活性的影响。结果表明:(1)高寒湿地不同湿地类型土壤微生物量和酶活性存在显著差异,其中SM土壤MBC、MBN、MBC\\N、QMB较S和M区高,对酶活性而言,SM和M区土壤蛋白酶和碱性磷酸酶活性较高,M区H2O2酶和脲酶活性较高。(2)氮添加显著增加了3种湿地类型中土壤MBC和MBN,其中MBC增加了7.00%-119.00%,MBN增加了8.03%-38.26%。氮添加仅显著增加了S和SM区土壤MBC/N和QMB (增加了24.68%-113.10%),但抑制了M区土壤MBC/N和QMB (抑制了8.93%-10.36%)。(3)氮添加显著增加了3种湿地类型土壤中脲酶、蛋白酶和H2O2酶活性,分别增加了7.25%-59.63%、4.71%-58.55%和34.70%-157.27%。但是氮添加对土壤碱性磷酸酶活性无显著影响。对蔗糖酶而言,N1处理增加了S区土壤蔗糖酶活性(增加了58.58%),而N2处理显著降低了22.72%。氮添加对SM和M区蔗糖酶活性无显著影响。(4)结构方程模型的结果显示,氮添加直接增加了土壤微生物量和酶活性。而随着湿地类型的变化(S-SM-M)直接和间接(通过pH)增加了酶活性;湿地类型的变化还通过影响pH、有机碳和有效养分间接增加了土壤微生物量。总之,氮添加和湿地类型可直接或间接的影响着土壤微生物量和酶活性。其中,土壤pH和有机碳是微生物量和酶活性变化的主要影响因素。本研究可为中亚干旱区高寒湿地应对未来气候变化的措施的制定提供技术参考。  相似文献   

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