中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
北京密云水库内湖消落带有机质、营养盐(氮/磷)含量分布特征

文献类型:期刊论文

作者秦丽欢; 曾庆慧; 李叙勇; 秦耀民
刊名湖泊科学
出版日期2016
卷号28期号:4页码:794-801
关键词消落带 有机质 密云水库 高程 土地利用 土壤深度
其他题名Distribution of organic matter and nutrient content in water-level-fluctuating zone of Miyun Reservoir inner lake, Beijing
中文摘要消落带是河流、湖泊和水库特有的一种现象,也是水陆生态系统间物质能量转换最活跃、最重要的区域,消落带的淹水-落干的频率和时间对消落带有机质和营养盐的形态转化与水界面的交换过程有重要影响.在密云水库的平水期(3月),对内湖消落带有机质、氮、磷含量分布进行调查,研究不同高程、土地利用和土壤深度的情况下,有机质和各营养盐含量的分布情况及相关关系,计算有机质和各营养盐在各高程下的储量,为消落带氮磷入库风险负荷量的评估,维护密云水库的水质安全提供依据.结果表明,密云水库内湖消落带有机质、总磷、总氮、氨氮、硝态氮、亚硝态氮和无机磷含量分别为23.1513.65 mg/g、0.170.09 mg/g、1.440.81 mg/g、10.863.54 mug/g、8.072.73 mug/g、0.410.71 mug/g、9.094.18 mug/g;土地利用情况对总氮、氨氮和硝态氮含量影响较大,而对有机质和总磷含量分布没有显著影响;在垂直分布上,有机质、总磷和总氮含量有随土壤深度增加而降低的趋势;利用相关分析得出有机质和土壤水分是影响氮、磷转化的重要因素;133~146 m高程范围内有机质、总磷和总氮的储量分别为5324.07、59.56和414.02 t.密云水库内湖消落带是有机质和营养盐的重要贮存库.
英文摘要Water-level-fluctuating zone (WLFZ) is a special phenomenon for rivers, lakes and reservoirs. It is also the most active and important zone for water and soil matter and energy exchange. The shifts between wet and dry period affects the nutrient transformation of WLFZ and water-soil exchange. In normal water season of Miyun Reservoir, the organic matter(OM) and nutrient content (N and P) of the water-level-fluctuating zone of inner lake was investigated,while the correlation among the soil physical chemical characteristics,OM and nutrient content was also be analyzed.Results indicated that the content of organic matter, total phosphorus, total nitrogen, ammonia nitrogen, nitrate nitrogen, inorganic phosphorus of inner lake of Miyun Reservoir was 23.1513.65 mg/g,0.170.09 mg/g,1.440.81 mg/g,10.863.54 mug/g,8.072.73 mug/g,0.410.71 mug/g,9.094.18 mug/g, respectively; Land use had impacts on content of total nitrogen, ammonia nitrogen, nitrate nitrogen, had no impact on the content of organic matter and total phosphorus. For the vertical distribution, organic matter, total phosphorus, total nitrogen all decreased with the soil depth increase. Correlation analysis showed that water content and organic matter were important factors for nitrogen and phosphorus transform. The reserve of organic matter, total nitrogen, total phosphorus in area between 133146 m was 5324.07, 59.56 and 414.02 t, respectively. So the water-lever-fluctuating zone was a very important OM and nutrient storage area. To keep the water quality, further studies about it were very necessary.
收录类别CSCD
CSCD记录号CSCD:5745828
源URL[http://ir.rcees.ac.cn/handle/311016/36453]  
专题生态环境研究中心_城市与区域生态国家重点实验室
推荐引用方式
GB/T 7714
秦丽欢,曾庆慧,李叙勇,等. 北京密云水库内湖消落带有机质、营养盐(氮/磷)含量分布特征[J]. 湖泊科学,2016,28(4):794-801.
APA 秦丽欢,曾庆慧,李叙勇,&秦耀民.(2016).北京密云水库内湖消落带有机质、营养盐(氮/磷)含量分布特征.湖泊科学,28(4),794-801.
MLA 秦丽欢,et al."北京密云水库内湖消落带有机质、营养盐(氮/磷)含量分布特征".湖泊科学 28.4(2016):794-801.

入库方式: OAI收割

来源:生态环境研究中心

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