石油开采产生的硫化氢沉积如何影响刚果沿海平原森林土壤的细菌群落和健康?

IF 2.1 Q3 SOIL SCIENCE
L. Koutika
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引用次数: 1

摘要

自1969年以来,石油开采产生的硫化氢(H2S)沉积可能会影响刚果沿海平原金合树和桉树种植园的细菌群落。这些人工林是在以前的原生稀树草原上实施的,目的是利用不适宜的土壤进行农业生产,提供纸浆木材和燃料木材能源,并保护天然林。据报道,与基线(桉树)储量相比,含有金合欢的林分的碳(C)和氮(N)储量有所增加。与天然稀树草原相比,造林林分中粗颗粒有机质(4000 - 250µm)的磷有效性也有所提高。利用16S rRNA细菌基因元条形码法对不同林分单种和混种林分的细菌门丰度进行了调查,结果显示放线菌在所有林分中都普遍存在。这一门通常与工业地区硫的存在有关,在有机物分解中起着至关重要的作用。这可能与土壤属性(碳、氮和磷)的改善有关,除了自然过程外,还与石油开采有关。因此,这篇综述显示了人类活动如何潜在地影响细菌群落组成,从而可能进一步改变其他土壤属性。它还承认,在天生营养贫乏的土壤上造林的可持续性在很大程度上依赖于土壤功能、环境和由土壤生物驱动的人类活动之间的相互作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
How hydrogen sulfide deposition from oil exploitation may affect bacterial communities and the health of forest soils in Congolese coastal plains?
The hydrogen sulfide (H2S) deposition from oil exploitation occurring since 1969 may potentially affect bacterial communities in acacia and eucalyptus plantations of the Congolese coastal plains. These plantations have been implemented on previous native savannas to use the unsuitable soils for agriculture, provide pulp wood and fuel wood energy, and preserve the natural forests. Increased carbon (C) and nitrogen (N) stocks in stands containing acacia relative to baseline (eucalyptus) stocks have been reported. Phosphorus availability also improved in coarse particulate organic matter (4,000–250 µm) in afforested stands as compared to natural savannas. Investigation of the abundance of bacterial phyla by metabarcoding of the 16S rRNA bacterial gene in different stands of monocultures and mixed-species stands reveals the prevalence of Actinobacteria in all stands. This phylum is generally associated with the presence of sulfur in industrial areas and has a crucial role in organic matter decomposition. This may be linked to improved soil attributes (C, N, and P) and related to oil exploitation in addition to natural processes. This review shows, therefore, how potentially human activities may impact bacterial community composition, which may further change other soil attributes. It also acknowledges that the sustainability of forest plantations on inherently nutrient-poor soils strongly relies on interactions between soil functions, the environment, and human activities driven by soil organisms.
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