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结合浓度梯度法和宏基因组学评估中国南方某石油污染黏土场地的天然源区耗竭情况

Assessing the Natural Source Zone Depletion of a Petroleum-Contaminated Clayey Soil Site in Southern China Combining Concentration Gradient Method and Metagenomics.

作者信息

Xu Zhe, Zhang Min, Ning Zhuo, He Ze, Zhang Fenge

机构信息

Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China.

School of Chinese Academy of Geological Sciences, China University of Geosciences, Beijing 100083, China.

出版信息

Life (Basel). 2024 Mar 4;14(3):337. doi: 10.3390/life14030337.

Abstract

Natural source zone depletion (NSZD) is the main process of LNAPL (Light Non-Aqueous Phase Liquid) removal under natural conditions. The NSZD rates assessed ranged from 0.55 to 11.55 kg·m·a (kilograms per square meter per year) in previous studies. However, most of these data were obtained from sandy sites, with few clayey sites. To gain knowledge of NSZD in clayey soil sites, the study assessed the NSZD of a petroleum hydrocarbon-contaminated clayey soil site in China, combining the concentration gradient method with metagenomic sequencing technology. The results show that the abundance of methane-producing key enzyme A gene in the source zone was more abundant than in background areas, which suggests that there was methanogenesis, the key process of NSZD. The concentration gradients of oxygen and carbon dioxide existed only in shallow soil (<0.7 m), which suggests that there was a thin methane oxidation zone in the shallow zone. The calculated NSZD rates range from 0.23 to 1.15 kg·m·a, which fall within the moderate range compared to previous NSZD sites. This study expands the knowledge of NSZD in clayey soil and enriches the attenuation rate data for contaminated sites, which is of significant importance in managing petroleum contaminants.

摘要

天然源区耗竭(NSZD)是自然条件下轻质非水相液体(LNAPL)去除的主要过程。在以往的研究中,评估的NSZD速率范围为0.55至11.55千克·米·年(每年每平方米千克数)。然而,这些数据大多来自砂质场地,粘质场地的数据很少。为了了解粘质土壤场地中的NSZD,本研究结合浓度梯度法和宏基因组测序技术,对中国一个受石油烃污染的粘质土壤场地的NSZD进行了评估。结果表明,源区中产甲烷关键酶A基因的丰度高于背景区域,这表明存在产甲烷作用,即NSZD的关键过程。氧气和二氧化碳的浓度梯度仅存在于浅层土壤(<0.7米)中,这表明浅层存在一个薄的甲烷氧化带。计算得出的NSZD速率范围为0.23至1.15千克·米·年,与之前的NSZD场地相比处于中等范围。本研究扩展了对粘质土壤中NSZD的认识,丰富了污染场地的衰减速率数据,这对管理石油污染物具有重要意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2a0e/10971796/71042484c67b/life-14-00337-g001.jpg

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