globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6025869
论文题名:
长江口芦苇湿地土壤酶活性对长期模拟升温的响应
其他题名: Responses of soil enzymatic activities to long-term simulated warming in Yangtze estuarine wetlands with Phragmites australis
作者: 高艳娜1; 戚志伟1; 仲启铖2; 李艳1; 姜楠1; 王开运1; 李沙沙1; 樊同1
刊名: 应用与环境生物学报
ISSN: 1006-687X
出版年: 2017
卷: 23, 期:3, 页码:442-459
语种: 中文
中文关键词: 土壤酶活性 ; 长期模拟升温 ; 季节变化 ; 土壤深度 ; 长江口 ; 芦苇湿地
英文关键词: soil enzyme activitiy ; long-term simulated warming ; seasonal change ; soil depth ; Yangtze estuarine ; Phragmites australis wetlands
WOS学科分类: AGRICULTURE MULTIDISCIPLINARY
WOS研究方向: Agriculture
中文摘要: 为促进气候变暖情景下长江口芦苇湿地可持续管理,以长江口崇明东滩芦苇湿地为对象,采用开顶室生长箱(Open top chamber, OTC)原位模拟大气温度升高,在升温的第8年研究芦苇湿地0-10 cm、 10-20 cm土层5种重要土壤酶(蔗糖酶、脲酶、酸性磷酸酶、中性磷酸酶和碱性磷酸酶)活性对长期模拟升温的响应. 结果显示:长达8年的连续升温显著提高了0-20 cm土层的土壤酶活性, 0-10 cm土层蔗糖酶、脲酶、酸性磷酸酶、中性磷酸酶和碱性磷酸酶活性分别增加71.9%、 84.7%、 41.8%、 105.7%和18.9%, 10-20 cm土层分别提高38.0%、 92.6%、 46.2%、 87.7%和34.0%. 升温与季节、土壤深度的交互作用对土壤酶活性影响显著. 春季(4月)0-10 cm土层蔗糖酶活性显著提高,但这一土层酸性磷酸酶、中性磷酸酶和碱性磷酸酶活性显著降低;夏季(7月)各土层的蔗糖酶、脲酶和中性磷酸酶活性显著提高;秋季(10月)各土层的5种土壤酶活性也显著提高;冬季(12月)各土层的5种土壤酶活性没有显著变化. 相关分析表明,土壤蔗糖酶、中性磷酸酶与土壤温度呈显著正相关, 5种土壤酶活性均与土壤有机碳呈显著正相关,土壤蔗糖酶、酸性磷酸酶和碱性磷酸酶与总磷也呈显著正相关. 综上表明,长期模拟升温能显著地改变长江口崇明东滩芦苇湿地土壤酶活性,进而可能影响这一地区的生态系统养分循环.
英文摘要: Soil enzymes are an important part of a wetland ecosystem. In this study, we evaluated the responses of soil enzymatic activities to long-term warming in relation to soil carbon, nitrogen, and phosphorus; this model has an important meaning in Yangtze Estuary Wetlands with Phragmites australis sustainable management under the conditions of climate warming. An in situ simulated warming experiment was conducted on the Eastern Chongming wetland with P. australis in the Yangtze Estuary; open-top chambers (OTCs) were applied to simulate climate warming. In the eighth year of warming, we studied the responses of several important soil enzymatic activities (invertase, urease, acid phosphatase, neutral phosphatase, and alkaline phosphatase) to long-term warming at soil depths of 0-10 and 10-20 cm. After eight years of continuous warming, the simulated warming signifcantly increased soil enzymatic activities at soil depths of 0-20 cm. The activities of invertase, urease, acid phosphatase, neutral phosphatase, and alkaline phosphatase increased by 71.9%, 84.7%, 41.8%, 105.7%, and 18.9%, respectively, at soil depths of 0-10 cm and increased by 38.0%, 92.6%, 46.2%, 87.7%, 34.0%, respectively, at soil depths of 10-20 cm. The effects of interaction of the warming, season, and soil depth on soil enzymatic activities were signifcant. The long-term simulated warming signifcantly improved spring (April) invertase activity at the 0-10 cm soil depth but signifcantly reduced soil acid phosphatase, neutral phosphatase, and alkaline phosphatase activities. The simulated warming signifcantly increased soil invertase, urease, and neutral phosphatase activities in the summer (July) at soil depths of 0-20 cm. In the autumn (October), fve soil enzymatic activities also signifcantly increased at two depths, but the long-term warming had no signifcant effect on fve soil enzymatic activities in winter (December). Correlation analysis revealed that invertase and neutral phosphatase activities signifcantly positively correlated with soil temperature; the activities of fve soil enzymes showed a signifcant positive correlation with soil organic carbon content; and invertase, acid phosphatase, and alkaline phosphatase activities signifcantly positively correlated with soil total phosphorus content. The long-term simulated warming signifcantly changed soil enzymatic activities; this alteration could have important effects on nutrient cycling in reed wetlands on Eastern Chongming Island in the Yangtze Estuary.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/153336
Appears in Collections:气候变化事实与影响

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作者单位: 1.华东师范大学生态与环境科学学院, 上海市城市化生态过程与生态恢复重点实验室, 上海 200241, 中国
2.上海市园林科学规划研究院, 上海 200232, 中国

Recommended Citation:
高艳娜,戚志伟,仲启铖,等. 长江口芦苇湿地土壤酶活性对长期模拟升温的响应[J]. 应用与环境生物学报,2017-01-01,23(3):442-459
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