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汞的形态分析及对土壤微生物活性的影响。

Mercury speciation and effects on soil microbial activities.

机构信息

College of Agricultural, Life and Natural Sciences, Department of Biological and Environmental Sciences, Alabama A&M University, Normal, Alabama 35762, USA.

出版信息

J Environ Sci Health A Tox Hazard Subst Environ Eng. 2012;47(6):854-62. doi: 10.1080/10934529.2012.665000.

Abstract

To study Hg toxicity on soil microbes and their activities, it is necessary to understand its various forms in soils. The objectives of this study were to investigate Hg speciation in four soil types spiked with Hg (300 mg kg(-1) soil) and its effects on soil microbial respiration and enzymes (amidohydrolases and phosphatase) activities. An assessment of the chemical forms, amounts, reactions, and mobility of Hg in soils and sediments is of significant importance to improve and maintain soil and environmental health and sustainability. Mercury speciation analysis was investigated under acidic and alkaline conditions using a modified sequential procedure, which differentiates Hg into the four distinct fractions. Soil microbial respiration and enzymes activities were determined under laboratory settings, by incubating the soils at 25°C for 30 days, and then determining the amount of CO(2) evolved. Speciation results revealed that the water soluble form was the least, with < 1% of the total Hg in the soil types investigated irrespective of the pH condition, while the residual fraction was the most abundant (> 80%) in Canisteo, Houston, and Ketona soils under acidic conditions and < 35% in Decatur soil. Under alkaline conditions, the residual fraction was ≤ 70% in Canisteo, Houston, and ketona and ≤ 29% in Decatur soil. The exchangeable fraction was the second most abundant fraction in the soils used ranging from 3.7-50.0% under acid conditions and 16.9-52.1% under alkaline conditions indicating that Hg desorption was found to be more favorable under alkaline than acidic conditions. Soil respiration was suppressed by Hg especially at the 100 mg kg(-1) concentration level. Amidohydrolases and phosphatases' response in the presence of Hg was variable. Amidohydrolases were more sensitive to Hg (18-90%) than phosphatase (0-35%) in all soils. This study demonstrated that the forms in which Hg exist in soils may determine its bioavailability and toxicity. Also microbial respiration and enzyme activities are potential bioindicators of heavy metal contamination of the environment.

摘要

为了研究汞对土壤微生物及其活性的毒性,有必要了解土壤中汞的各种形态。本研究的目的是研究四种添加汞(土壤 300mgkg(-1))的土壤类型中的汞形态及其对土壤微生物呼吸和酶(酰胺水解酶和磷酸酶)活性的影响。评估土壤和沉积物中汞的化学形态、数量、反应和迁移性,对于改善和维持土壤和环境健康与可持续性具有重要意义。采用改良的顺序提取法,在酸性和碱性条件下研究了汞的形态分析,该方法将汞分为四个不同的部分。在实验室条件下,通过在 25°C 下培养土壤 30 天,然后测定释放的 CO2 量,来确定土壤微生物呼吸和酶活性。形态结果表明,水溶性形态最少,在所研究的土壤类型中,不论 pH 条件如何,其含量均低于总汞的 1%,而在酸性条件下,Canisteo、Houston 和 Ketona 土壤中残余部分最丰富(>80%),Decatur 土壤中则<35%。在碱性条件下,Canisteo、Houston 和 Ketona 土壤中的残余部分≤70%,Decatur 土壤中的残余部分≤29%。在所用的土壤中,交换态部分是第二丰富的部分,在酸性条件下为 3.7-50.0%,在碱性条件下为 16.9-52.1%,这表明在碱性条件下,Hg 的解吸更有利。汞尤其在 100mgkg(-1)浓度水平下抑制土壤呼吸。在存在汞的情况下,酰胺水解酶和磷酸酶的反应是可变的。在所有土壤中,酰胺水解酶对汞的敏感性(18-90%)高于磷酸酶(0-35%)。本研究表明,土壤中汞的存在形式可能决定其生物利用度和毒性。此外,微生物呼吸和酶活性可能是重金属污染环境的潜在生物标志物。

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