Post-fire changes in soil extracellular enzyme activities and their influencing factors in the permafrost region of the Da Xing'anling Mountains, Northeast China.

Q3 Environmental Science
Yang Shen, Xiao-Ying Li, Hui-Ying Cai, Tao Xu, Jing-Tao Li, Kui Chen
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Abstract

Understanding the changes in soil enzyme activities and the influencing factors after forest fire distur-bances can help assess and predict the impacts of climate warming on permafrost ecosystems. We analyzed the acti-vities of extracellular enzyme, including urease (UR), acid phosphatase (AP), acetyl-glucosidase (NAG), β-glucosidase (βG), and leucine aminopeptidase (LAP), in soils (0-60 cm depth) across unburned, lightly burned and severely burned sites within the 2015 burned area in the northern Da Xing'anling Monntains. The results showed that fire intensity, soil depth, and soil physicochemical properties significantly influenced extracellular enzyme activities. Compared to that in unburned site, the activities of UR, AP, βG, and LAP increased by 59.8%-241.7%, while NAG decreased by 35.5% at lightly burned site. The activities of all soil enzymes increased, with the magnitidues ranging from 26.0% to 206.0% at severely burned site. Soil enzyme activities gra-dually decreased with increasing soil depth. Redundancy analysis identified soil temperature (ST), total phosphorus (TP), C:P, C:N, soil depth and soil water content (SWC) as important influencing factors of soil enzyme activities, contributing 70.9%, 12.2%, 4.7%, 3.6%, 2.9%, and 1.9%, respectively. Soil enzyme activities were signifi-cantly positively correlated with ST, TP, C:P, C:N, and SWC, but significantly negatively correlated with soil depth. Forest fires and the resultant changes in soil physicochemical properties jointly affected soil extracellular enzyme activities, with the effects intensifying with increasing fire intensity.

火灾后大兴安岭多年冻土区土壤胞外酶活性变化及其影响因素
了解森林火灾扰动后土壤酶活性的变化及其影响因素,有助于评估和预测气候变暖对冻土生态系统的影响。研究了2015年大兴安岭北麓3处未烧、轻烧和重度烧样土壤(0 ~ 60 cm深度)胞外酶脲酶(UR)、酸性磷酸酶(AP)、乙酰-葡萄糖苷酶(NAG)、β-葡萄糖苷酶(βG)和亮氨酸氨基肽酶(LAP)的活性。结果表明,火灾强度、土壤深度和土壤理化性质对胞外酶活性有显著影响。与未燃烧位点相比,轻度燃烧位点UR、AP、βG和LAP活性升高59.8% ~ 241.7%,NAG活性降低35.5%。所有土壤酶活性均有所增加,严重烧伤地的增幅为26.0% ~ 206.0%。土壤酶活性随土层深度的增加而逐渐降低。冗余分析表明,土壤温度(ST)、全磷(TP)、C:P、C:N、土壤深度和土壤含水量(SWC)是土壤酶活性的重要影响因子,对土壤酶活性的贡献率分别为70.9%、12.2%、4.7%、3.6%、2.9%和1.9%。土壤酶活性与ST、TP、C:P、C:N和SWC呈极显著正相关,与土壤深度呈极显著负相关。森林火灾及其引起的土壤理化性质变化共同影响土壤胞外酶活性,且随火灾强度的增加而增强。
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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
自引率
0.00%
发文量
11393
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