位置:成果数据库 > 期刊 > 期刊详情页
中国生态系统研究网络水体pH和矿化度监测数据初步分析
  • ISSN号:1001-8166
  • 期刊名称:地球科学进展
  • 时间:0
  • 页码:1042-1050
  • 语言:中文
  • 分类:X832[环境科学与工程—环境工程]
  • 作者机构:[1]中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室, [2]CERN水分分中心,北京100101
  • 相关基金:基金项目:中国科学院知识创新工程重要方向项目“长期生态监测数据质量控制与数据开发的方法和关键技术研究一水分监测质量控制方法研究与数据产品开发”(编号:KZCX2.YW-433-01);国家自然科学基金面上项目“土壤和气候因素对森林生态系统土壤有机碳的影响”(编号:30600091)和“氮沉降对长白山典型温带森林土壤碳动态影响实验研究”(编号:40701186)资助.
  • 相关项目:氮沉降对长白山典型温带森林土壤碳动态影响实验研究
中文摘要:

介绍了中国生态系统研究网络(CERN)陆地生态系统水环境监测指标与频率。初步分析了CERN31个典型陆地生态系统监测地表水和地下水、6个湖泊和海湾生态系统、1个城市生态系统地下水体pH、矿化度(电导率)状况。结果表明,我国森林生态系统pH和矿化度分布规律基本一致,为从西向东、从北向南逐渐降低的趋势,pH在鼎湖山自然保护区出现强酸性(4.15),其他台站为弱碱性、中性或弱酸性(6.01~8.26),森林生态系统矿化度均较低(33~322mg/L)。我国农田、荒漠、湿地生态系统水体pH和矿化度分布规律为:华北与黄土农业区、西北绿洲农业与牧业区相对较高,东北农业区和青藏高原农牧区其次,南方农业区最低;除南方农业生态系统与北方三江湿地生态系统水体pH为弱酸性(6.27~6.82)外,其他监测水体均为中性和弱碱性,500mg/L以上矿化度水体主要出现在西北部荒漠生态系统,黄河冲积平原农业生态系统。湖泊、海湾生态系统水体和北京城市生态系统地下水pH均为弱碱性,海湾水体pH季节波动不明显,湖泊水体和北京城市地下水pH和电导率呈明显季节波动,湖泊水体pH表现为夏秋季节较高,电导率表现为6~9月较低;北京城市地下水pH为5~10月较低,矿化度(电导率)为5~7月较高。建议未来水体pH和矿化度(电导率)采取传感器原位高频率监测、在坚持长期定位监测同时增加区域调查、结合科学问题开展监测和研究,提高监测数据回答水质长期变化趋势、区域尺度人类活动影响的能力。

英文摘要:

The water quality monitoring index and frequency of typical terrestrial ecosystem on the Chinese E- cosystem Research Network (CERN) were reviewed. Furthermore, the water pH and salinity of the 31 typical terrestrial ecosystems during 2004 to 2006, of the 6 lake and bay ecosystems during 2003-2007, and of one urban ecosystem during 2008 were assessed. The results showed : (1)The pH and salinity of the CERN forest ecosystems decreased from northern to southern ecosystems and from western to eastern ecosystems. The lowest pH value was in the southeast Dinghu forest ecosystem (4.15), while the pH value ranged from 6.01 to 8.26 in the other forest ecosystems. The salinity ranged from 33 to 322 mg/L in the forest ecosystems. (2)The pH and salinity of the CERN agriculture-, oasis-, and marsh-ecosystem had obvious spatial trends, with the higher values in the North China Plain, Northwest oasis and desert area, the lower values in the northeast agricultural area and the lowest values in the southern agricultural area. The pH ranged from 6.70 to 8.45 except those in Sanjiang marsh ecosystem and southern agricultural ecosystems with the lower pH values. The higher salinity values (more than 500 mg/L) were mainly in the western oasis and Yellow River floodplain agricultural ecosystems. (3)The pH in the lake, bay and Beijing urban underground water were ranged from 6.8 to 8.8. There was little seasonal variation of pH in the bay sites hut significant seasonal variation of pH and electrical conductivity in the lake sites and Beijing urban underground water. In the lake sites, the pH values were higher in summer and autumn, but the electrical conductivity values were lower during June to September. While in the underground water of Beijing urban site, the pH values were lower during May to October, while the salinity ( electrical conductivity) values were higher during May to July. The study suggests that the advanced in-situ remote sensor technique, with high monitoring frequency, he n

同期刊论文项目
同项目期刊论文
期刊信息
  • 《地球科学进展》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国科学院资源环境科学与技术局 国家自然科学基金委员会地球科学部 中国科学院资源环境科学信息中心
  • 主编:傅伯杰
  • 地址:兰州市天水中路8号
  • 邮编:730000
  • 邮箱:adearth@lzb.ac.cn
  • 电话:0931-8762293
  • 国际标准刊号:ISSN:1001-8166
  • 国内统一刊号:ISSN:62-1091/P
  • 邮发代号:54-86
  • 获奖情况:
  • 国家“双效”期刊,甘肃社优秀期刊,中国数字化优秀期刊
  • 国内外数据库收录:
  • 美国化学文摘(网络版),日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版)
  • 被引量:36043