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热带沼泽地中某菌株对石油卤水污染土壤的修复

Recovery of Petroleum Brine-Contaminated Soil by sp. in a Tropical Marshland.

作者信息

Domínguez-Rodríguez Verónica Isidra, Guzmán-Osorio Francisco J, Hernández-Acosta Liliana, Gómez-Cruz Rodolfo, Rosique-Gil J Edmundo, Adams Randy H

机构信息

Academic Division of Biological Sciences, Remediation Laboratory, Universidad Juárez Autónoma de Tabasco, Carretera Villahermosa-Cárdenas Km. 0.5 S/N, Villahermosa, Tabasco 86150, México.

National Technology of Mexico / ITS of Comalcalco, Carretera Vecinal Comalcalco - Paraíso Km. 2, Ra. Occidente 3ra. Sección Comalcalco, Tabasco C.P. 86651, México.

出版信息

Trop Life Sci Res. 2024 Jul;35(2):141-165. doi: 10.21315/tlsr2024.35.2.7. Epub 2024 Jul 31.

DOI:10.21315/tlsr2024.35.2.7
PMID:39234474
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11371406/
Abstract

Almost all research on natural attenuation and phytoremediation of sites contaminated with briny produced water has been conducted in temperate climates, however, there is a dearth of information on the use of tropical species for this purpose. It is within this context, that we investigated a spontaneously growing hypersaline spikerush from a contaminated site in southeast Mexico, to determine its soil salinity limits, the relationship between soil organic matter and salinity, and for preliminary documentation of floristic succession with sp. for phytoremediation o f brine s pills. Soil was sampled (0 cm-20 cm) three times between 2018-2021, focusing on the end of the dry season (most critical period). The species tentatively identified as was tolerant to soil hypersalinity (Electrical Conductivity: 125 dS/m) and appeared to generate a cyclic process of succession to recover areas with soil salinity levels higher than it could otherwise tolerate. A salinity gradient was found between the most heavily contaminated part of the site ("kill zone", > 212 dS/m), the first sp. individuals (125 dS/m), slowly advancing through the main spikerush stand, and finally into a cattail stand (< 8.02 dS/m). Similarly, an inverse relationship between Soil Organic Matter content and soil salinity was observed. This is the first time this species has been identified with a brine spill, its salinity limits determined, and investigated for use in phytoremediation of this kind.

摘要

几乎所有关于受含盐采出水污染场地的自然衰减和植物修复的研究都是在温带气候下进行的,然而,关于为此目的使用热带物种的信息却很匮乏。正是在这种背景下,我们对一种从墨西哥东南部受污染场地自然生长的超盐生碱蓬进行了调查,以确定其土壤盐分限度、土壤有机质与盐分之间的关系,并初步记录该物种在盐水泄漏植物修复中的植物演替情况。在2018年至2021年期间对土壤(0厘米至20厘米)进行了三次采样,重点是旱季末期(最关键时期)。初步鉴定为该物种的植物能够耐受土壤高盐度(电导率:125 dS/m),并且似乎产生了一个循环演替过程,以恢复土壤盐分水平高于其正常耐受水平的区域。在该场地污染最严重的部分(“死亡区”,> 212 dS/m)、第一批该物种个体(125 dS/m)、缓慢推进穿过主要碱蓬林分,最后进入香蒲林分(< 8.02 dS/m)之间发现了一个盐分梯度。同样,观察到土壤有机质含量与土壤盐分之间呈反比关系。这是首次鉴定出该物种与盐水泄漏有关,确定了其盐分限度,并对其在这类植物修复中的应用进行了研究。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/d799c49c70b2/TLSR-35-2-141-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/a3b9ed35f6f0/TLSR-35-2-141-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/b661a4a734cf/TLSR-35-2-141-g002.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/08615e0421d4/TLSR-35-2-141-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/bec3f02f3524/TLSR-35-2-141-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/8d924bb1f0d3/TLSR-35-2-141-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/24026bb71c32/TLSR-35-2-141-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/d799c49c70b2/TLSR-35-2-141-g009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/a3b9ed35f6f0/TLSR-35-2-141-g001.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/2e57061e8c19/TLSR-35-2-141-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/8df41c5f00ae/TLSR-35-2-141-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/08615e0421d4/TLSR-35-2-141-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/bec3f02f3524/TLSR-35-2-141-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/8d924bb1f0d3/TLSR-35-2-141-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/24026bb71c32/TLSR-35-2-141-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/356b/11371406/d799c49c70b2/TLSR-35-2-141-g009.jpg

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本文引用的文献

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