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《辽宁城乡环境科技》2009,(9):15-15
湖北省神农架国家大气背景站建设近日全面启动,通路、通水、通电、通讯和场地平整工程开工建设。据了解,按照原来的公路建设方案,几十株秦岭冷杉和巴山冷杉要被砍伐。为了保护国家二级树种和生态环境,神农架林区环境保护局报请湖北省环境保护厅,决定改变建设方案,公路建设绕过古树。目前,背景站主站房主体工程进入实地勘测阶段,按进度要求,10月底工程建设全部完成并接受验收,随后进行仪器安装。 相似文献
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1999年与2014年贡嘎山峨眉冷杉枝和叶中常见重金属的生物富集特征对比 总被引:1,自引:0,他引:1
经济的快速发展使得生态环境的承载力日益接近上限,而关于偏远地区森林系统的重金属污染的时间变化趋势却鲜有报道.本文测定了贡嘎山1999年与2014年采集的峨嵋冷杉枝、叶中的Pb、Hg、Cr、As、Cd、Mn、Cu、Zn与Ba.结果表明:11999年枝、叶样品中Pb、Hg、As、Cd、Mn与Cu显著高于2014年的量,而2014年枝、叶样品中Cr、Zn和Ba高于1999年的量;2枝中Pb、Hg、Cr、As、Cd、Mn、Cu、Zn和Ba与生长龄无统一的变化趋势,而在叶中的含量随着生长龄的增加有增加的趋势;3Hg易在叶中富集,而其它元素更易在枝中富集;通过在主成分分析的基础上进行多元线性回归判断常见重金属元素的来源,枝、叶中的Pb、Cr、As、Cd、Cu、Zn和Ba有42.3%~92.2%的含量来自于土壤,而枝、叶中的Hg有70.6%的含量来自于大气.这说明Hg存在与其他重金属在森林系统不同的累积机制. 相似文献
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峨嵋山冷杉林大面积死亡已发现多年,大多数学者认为其原因是酸沉降和高位沼泽化,但缺乏定量研究。为进一步研讨酸沉降与高位沼泽对峨嵋山冷杉衰亡的影响,1995年两次展开了调查,调查结果表明,峨嵋山太子坪一带(海拔2858m),由于泥炭的过度发育和大量堆积,形成高位沼泽,使土壤渍水严重,透气性变差,使冷杉根的正常生长受损;加之有毒元素Al在冷杉体内富集,抑制了冷杉对营养元素Ca,Mg等的吸收,导致冷杉秃顶 相似文献
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Streamwater chemistry and flow dynamics along vegetation-soil gradient in a subalpine Abies fabri forest watershed, China 总被引:1,自引:0,他引:1
Streamwater chemistry and spatial flow dynamics from a subalpine Abies fabri forest in an experimental watershed located in the east slope of Gongga Mountain were analyzed to gain insights into the gradient effect of primary community succession on the stream biogeochemical process. Results showed that high sand content (exceeding 80%) and porosity in the soil(exceeding 20% in A horizon and 35% in B horizon), as well as a thick humus layer on the soil surface, made the water exchange quickly in the Huangbengliu (HBL) watershed. Consequently, no surface runoff was observed, and the stream discharge changed rapidly with the daily precipitation. The flow trends of base ions in the stream water were influenced by the Abies fabri succession gradient. Ca^2 , HCO3^- and SO4^2,- were the dominant anions in the streamwater in this region. A significant difference of Ca^2 , HCO3^- and SO4^2- concentration exported between the succession stages in the watershed can be found. But they had the similar temporal change in the stream flow. Ca^2 , HCO3^- and SO4^2- showed significantly negative correlations with the daily precipitation and the stream discharge. Concentrations of Cl^- , Na^ , K^ , and Mg^2 were low in all streamwaters monitored and we observed no differences along the Abies fabri succession gradient. Low ratios of Na. (Na Ca) (range from 0.1 to 0.2) implied cations were from bedrock weathering (internal source process in the soil system) in this region. But, a variance analysis showed there were almost no differences between rainwater and streamwaters for Mg^2 , Na^ , K^ , and Cl^- concentrations. This indicated that they might be come from rainfall inputs(external source). The highly mobile capacity, rapid water exchange between precipitation and discharge, and long-term export lead to this observed pattern were suggested. 相似文献
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