干旱区露天煤矿开采对土壤酶活性和微生物代谢限制的影响
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1.新疆师范大学生命科学学院 新疆特殊环境物种保护与调控生物试验室;2.中国科学院新疆生态与地理研究所 干旱区生态安全与可持续发展全国重点实验室;3.新疆干旱区生物多样性保育与应用重点实验室;4.新疆天池能源有限责任公司

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新疆维吾尔自治区重大科技专项(2023A01002)


Effects of open-pit coal mining on soil enzyme activities and microbial metabolic limitations in arid area
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1.Key Laboratory of Special Species Conservation and Regulatory Biology, College of Life Sciences, Xinjiang Normal University, Urumqi 830017, China;2.State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;3.Xinjiang Key Laboratory of Biodiversity Conservation and Application in Arid Lands, Urumqi 830011, China

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    摘要:

    干旱区生态系统本底脆弱,煤矿开采后的生态修复一直是恢复生态学领域的核心研究课题。然而,干旱区露天煤矿开采将如何影响矿坑周围土壤酶活性和微生物代谢限制,这种影响是否会随距离矿坑的远近和方向存在差异等科学问题还尚不清楚。基于此,本研究以新疆准东煤矿区为典型研究区,系统采集矿坑周边8个方位、11个距离梯度及对照区(CK)0-10 cm的土壤样品;系统测定了土壤理化性质及微生物代谢关键酶活性:碳(C)获取酶:β-1,4-葡萄糖苷酶(BG);氮(N)获取酶:β-1,4-N-乙酰氨基葡萄糖苷酶(NAG)和亮氨酸氨基肽酶(LAP);磷(P)获取酶:碱性磷酸酶(AKP),并结合多种分析方法开展深入解析。结果表明:露天煤矿开采显著改变了土壤酶活性的空间分布格局,呈现明显异质性特征:BG、NAG和LAP活性在矿坑近周边形成高值聚集区,AKP活性则随距矿坑距离的增加呈逐步升高趋势;且酶活性对开采扰动的响应存在显著风向差异,下风向(DW)与上风向(UW)表现出差异化规律。具体而言,DW C获取酶活性显著高于UW,而P获取酶活性显著低于UW及CK;各风向C、P获取酶活性均低于CK,N获取酶活性在不同风向及与CK相比均无显著差异。生态酶向量模型分析显示,矿区土壤微生物代谢普遍受到N、P元素的共同限制:DW以P限制为主导,UP则兼具N限制与P限制双重特征;同时发现,煤矿开采显著降低了微生物的C限制程度。冗余分析与随机森林模型结果进一步揭示,全氮(TN)是调控研究区整体及UP微生物代谢限制的核心驱动因子,而DW微生物代谢限制则受速效磷(AP)调控。

    Abstract:

    The arid ecosystem is inherently fragile, and ecological restoration after coal mining has long been a core research topic in the field of restoration ecology. However, key scientific questions remain elusive, such as how open-pit coal mining in arid regions affects soil enzyme activities and microbial metabolic limitations in the vicinity of mining pits, and whether such impacts vary with the distance from the pits and sampling directions. Therefore, the study focused on the Zhundong coal mining area in Xinjiang as a typical research area.Soil samples(0–10 cm) were systematically collected from 11 distance gradients across 8 directions around the mining pit, as well as from the control area. We systematically determined soil physicochemical properties and the activities of key enzymes involved in microbial metabolism, including carbon (C)-acquiring enzyme: β-1,4-glucosidase (BG); nitrogen (N)-acquiring enzymes: β-1,4-N-acetylglucosaminidase (NAG) and leucine aminopeptidase (LAP); and phosphorus (P)-acquiring enzyme: alkaline phosphatase (AKP). In addition, in-depth analysis was carried out by combining multiple analytical methods. Results showed that open-pit coal mining significantly altered the spatial distribution pattern of soil enzyme activities, which exhibited obvious heterogeneity characteristics: the activities of BG, NAG, and LAP formed high-value aggregation areas in the immediate vicinity of the mining pit, while AKP activity increased gradually with the increasing distance from it; moreover, there were significant wind direction differences in the response of enzyme activities to mining disturbance, with differential patterns observed between the downwind (DW) and upwind (UW) directions. More specifically, the activity of C-acquiring enzymes in the downwind (DW) direction was significantly higher than that in the upwind (UW) direction, while the activity of P-acquiring enzymes in the DW direction was significantly lower than that in both the UW direction and the control area (CK). Additionally, the activities of C- and P-acquiring enzymes in all wind directions were lower than those in the CK area. In contrast, there were no significant differences in N-acquiring enzyme activity across different wind directions or compared with the CK area. Analysis using the ecoenzymatic stoichiometry model showed that soil microbial metabolism in the mining area was generally co-limited by N and P: microbial metabolism in the DW direction was dominated by P limitation, while that in the UW direction exhibited dual characteristics of both N limitation and P limitation. Meanwhile, it was found that open-pit coal mining significantly reduced the degree of C limitation on microorganisms. Redundancy analysis and random forest model further revealed that total nitrogen (TN) was the core driving factor regulating the overall microbial metabolic limitations in the study area and those in the upwind (UW) direction. In contrast, the microbial metabolic limitations in the downwind (DW) direction were primarily regulated by available phosphorus (AP).

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韩志立,尹本丰,杨傲,张庆,杨志勇,黄韵杰,张署军,王菲菲,张静,乔云娜,李奇奇,陈德付,胡桂林,马晓东,张元明,臧永新.干旱区露天煤矿开采对土壤酶活性和微生物代谢限制的影响.生态学报,,(). http://dx. doi. org/10.5846/stxb202512213413

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