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三江平原小叶章钾、钙、镁含量与累积的季节变化
引用本文:孙志高,刘景双,于君宝,陈小兵. 三江平原小叶章钾、钙、镁含量与累积的季节变化[J]. 应用生态学报, 2009, 20(5): 1051-1059
作者姓名:孙志高  刘景双  于君宝  陈小兵
作者单位:1.中国科学院烟台海岸带可持续发展研究所, 山东烟台 264003;2.中国科学院东北地理与农业生态研究所, 长春 130012
基金项目:国家自然科学基金,中国科学院知识创新工程重要方向性项目,中国科学院百人计划项目,山东省黄河三角洲生态环境重点实验室开放基金,中国科学院优秀博士学位论文、院长奖获得者科研启动专项基金 
摘    要:2004年5—10月,对三江平原典型小叶章草甸和小叶章-苔草沼泽化草甸群落优势植物小叶章的K、Ca、Mg含量与累积的季节变化进行了研究.结果表明:典型草甸和沼泽化草甸小叶章不同器官K、Ca、Mg含量差异较大,其中,其地上器官的K含量整体均呈下降趋势,符合线性模型(y=A+Bt);茎中Ca含量变幅不大,符合抛物线模型(y=A+B1t+B2t2),叶和叶鞘中整体呈递增变化,符合指数增长模型(y=Aexp(t/B1)+B2);茎中Mg含量变幅最大,而叶和叶鞘相对平缓.不同时期小叶章各器官K、Ca、Mg含量差异较大,典型草甸小叶章地上器官的K含量大多高于沼泽化草甸小叶章,而沼泽化草甸小叶章根、叶鞘的Ca、Mg含量则高于典型草甸小叶章;典型草甸和沼泽化草甸小叶章不同器官K、Ca、Mg储量及累积速率差异明显,其中根的储量最大,分别占总储量的(63.82±23.19)%、(78.68±15.44)%、(76.48±19.06)%和(85.23±9.20)%、(93.51±3.46)%、(92.39±3.22)%.典型草甸小叶章地上器官K、Ca、Mg储量均明显高于沼泽化草甸小叶章,根则相反.这种差异主要与小叶章生态学特性及所处生境有关。

关 键 词:再生水回灌  地下水水质  盐分  氮素  重金属  有机污染物  病原微生物  
收稿时间:2008-08-24

Seasonal changes of potassium, calcium and magnesium contents and accumulation in Calamagrostis angustifolia in Sanjiang Plain.
SUN Zhi-gao,LIU Jing-shuang,YU Jun-bao,CHEN Xiao-bing. Seasonal changes of potassium, calcium and magnesium contents and accumulation in Calamagrostis angustifolia in Sanjiang Plain.[J]. The journal of applied ecology, 2009, 20(5): 1051-1059
Authors:SUN Zhi-gao  LIU Jing-shuang  YU Jun-bao  CHEN Xiao-bing
Affiliation:1.Yantai Institute of Coastal Zone Research for Sustainable Development, Chinese Academy of Sciences, Yantai 264003, Shandong, China;2.Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130012, China
Abstract:From May to October 2004, the seasonal changes of K, Ca, and Mg contents and accumulation in Calamagrostis angustifolia, the dominant species in the typical meadow and marsh meadow communities of Sanjiang Plain, were studied. There was a greater difference in the seasonal changes of K, Ca, and Mg contents in different parts of typical meadow C. angustifolia (TMC) and marsh meadow C. angustifolia (MMC). The K content in aboveground parts of the two communities had an overall decreasing trend, according with linear model K=A+Bt, the Ca content had a smaller change in stem but an overall increasing trend in leaf and vagina, being accorded with parabola model Ca=A+B1t+B2t2 and exponential growth model Ca=Aexp(t/B1)+B2, respectively, while the Mg content had the greatest change in stem but changed relatively smoothly in leaf and vagina. The differences of K, Ca, and Mg contents in different parts of TMC and MMC were obvious. The K content in aboveground parts of TMC was generally higher than that of MMC, while the Ca and Mg contents in the root and vagina of MMC were higher than those of TMC. The K, Ca, and Mg storage and accumulation in different parts of TMC and MMC also differed. Root had the greatest K, Ca, and Mg storage, occupying 6382±2319%, 7868±15.44%, and 7648±1906% of the total storage in TMC and 8523±920%, 9351±346%, and 9239±322% in MMC, respectively. The aboveground parts of TMC had a higher storage of K, Ca and Mg than those of MMC, while the root was in adverse. Such a difference was mainly due to ecological characteristics of C. angustifolia and its habitat conditions.
Keywords:reclaimed water recharge   groundwater quality   salt   nitrogen   heavy metal   organic contaminant   pathogen.  
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