College of Forestry, Gansu Agricultural University, Lanzhou, 730070, China.
School of Science and the Environment, Memorial University of Newfoundland, 20 University Drive, Corner Brook, NL, A2H 5G4, Canada.
Sci Rep. 2020 Dec 4;10(1):21271. doi: 10.1038/s41598-020-78182-9.
Vegetation degradation, due to climate change and human activities, changes the biomass, vegetation species composition, and soil nutrient input sources and thus affects soil nutrient cycling and enzyme activities. However, few studies have focused on the responses of soil nutrients and enzymes to vegetation degradation in high-altitude wet meadows. In this study, we examined the effects of vegetation degradation on soil nutrients (soil organic carbon, SOC; total nitrogen, TN; total phosphorus, TP) and enzyme activities (i.e., urease, catalase, amylase) in an alpine meadow in the eastern margin of the Qinghai-Tibet Plateau. Four different levels of degradation were defined in terms of vegetation density and composition: primary wet meadow (CK), lightly degraded (LD), moderately degraded (MD), and heavily degraded (HD). Soil samples were collected at depth intervals of 0-10, 10-20, 20-40, 40-60, 60-80, and 80-100 cm to determine soil nutrient levels and enzyme activities. The results showed that SOC, TN, catalase and amylase significantly decreased with degradation level, while TP and urease increased with degradation level (P < 0.05). Soil nutrient and enzyme activity significantly decreased with soil depth (P < 0.05), and the soil nutrient and enzyme activity exhibited obvious "surface aggregation". The activities of soil urease and catalase were strongest in spring and weakest in winter. The content of TN in spring, summer, and autumn was significantly higher than observed in winter (P < 0.05). The soil TP content increased in winter. Soil amylase activity was significantly higher in summerm than in spring, autumn, and winter (P < 0.05). TP was the main limiting factor for plant growth in the Gahai wet meadow. Values of SOC and TN were positively and significantly correlated with amylase and catalase (P < 0.05), but negatively correlated with urease (P < 0.05). These results suggest the significant role that vegetation degradation and seasonal freeze-thaw cycle play in regulating enzyme activities and nutrient availability in wet meadow soil.
植被退化受气候变化和人类活动的影响,改变了生物量、植被物种组成以及土壤养分输入源,从而影响土壤养分循环和酶活性。然而,很少有研究关注高海拔湿地植被退化对土壤养分和酶的影响。在这项研究中,我们研究了青藏高原东缘高寒草甸植被退化对土壤养分(土壤有机碳(SOC)、总氮(TN)、总磷(TP))和酶活性(即脲酶、过氧化氢酶、淀粉酶)的影响。根据植被密度和组成,将退化程度分为 4 个等级:原生湿地(CK)、轻度退化(LD)、中度退化(MD)和重度退化(HD)。在 0-10、10-20、20-40、40-60、60-80 和 80-100cm 的深度间隔采集土壤样本,以确定土壤养分水平和酶活性。结果表明,随着退化程度的增加,SOC、TN、过氧化氢酶和淀粉酶显著降低,而 TP 和脲酶则增加(P<0.05)。土壤养分和酶活性随土壤深度显著降低(P<0.05),土壤养分和酶活性表现出明显的“表面聚集”。土壤脲酶和过氧化氢酶的活性在春季最强,冬季最弱。春、夏、秋季 TN 含量显著高于冬季(P<0.05)。冬季土壤 TP 含量增加。夏季土壤淀粉酶活性显著高于春季、秋季和冬季(P<0.05)。TP 是嘎海湿地植物生长的主要限制因素。SOC 和 TN 值与淀粉酶和过氧化氢酶呈显著正相关(P<0.05),但与脲酶呈显著负相关(P<0.05)。这些结果表明,植被退化和季节性冻融循环在调节湿地土壤酶活性和养分供应方面发挥了重要作用。