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131.
辽东山地老秃顶子冰缘地貌植物群落类型及基本特征 总被引:3,自引:0,他引:3
基于48个样地的群落调查数据,运用TWINSPAN分类方法,对辽东山地老秃顶子冰缘地貌植物群落类型进行了划分,并对群落结构、种类组成和生活型谱进行了系统研究.结果表明:老秃顶子冰缘地貌植被可划分为16个森林群系、6个灌丛群系,归并为落叶阔叶林、针阔混交林、暗针叶林、矮曲林、灌丛、灌草丛6个植被型.其中,石海地貌主要发育灌丛和灌草丛,也有针阔混交林和矮曲林分布;石河地貌主要发育针阔混交林和落叶阔叶林,也有暗针叶林分布;石流坡地貌主要发育针阔混交林、落叶阔叶林和灌丛,也有矮曲林分布.老秃顶子冰缘地貌植被由68科138属193种维管束植物组成;石海与石河间植物群落物种组成属中等不相似,而石河与石流坡间属中等相似.老秃顶子冰缘地貌植物群落中高位芽植物占38.0%,隐芽植物占36.3%,地面芽植物占21.8%,地上芽植物和一年生植物均很少,反映出辽东山地冰缘地貌区具有夏季温暖多雨、冬季寒冷漫长的气候特点.相对而言,石海、石流坡地貌中隐芽植物较多,石河地貌中高位芽植物较多,表明石海、石流坡地貌具有更为冷湿的小气候环境. 相似文献
132.
建立异质性农户土地流转行为的理论分析基础,利用Logistic回归分析方法和河南省调查数据,明确农户土地流转决策的影响因素。研究结果表明:农村信贷市场约束是纯农户、以农业收入为主的农户转入土地的需求不足的重要原因;规避就业风险和争夺土地租金是非农户和以非农业收入为主的农户转出土地的供给不足的主要原因;土地控制权偏好与生存预期造成中年、老年农户竭力排斥土地流转;农村土地流转不活跃的决定性因素是国家保护农业与有效管理兼业农户、非农户的责任缺位。 相似文献
133.
《Chemie der Erde / Geochemistry》2015,75(2):261-270
The aim of this study was to investigate the accumulation of arsenic (As) in and on roots of Zea mays (maize) and Helianthus annuus (sunflower) by means of synchrotron-based micro-focused X-ray fluorescence imaging (μ-XRF). Plant and soil samples were collected from two field sites in the Hetao Plain (Inner Mongolia, China) which have been regularly irrigated with As-rich groundwater. Detailed μ-XRF element distribution maps were generated at the Fluo-beamline of the Anka synchrotron facility (Karlsruhe Institute of Technology) to assess the spatial distribution of As in thin sections of plant roots and soil particles. The results showed that average As concentrations in the roots (14.5–27.4 mg kg−1) covered a similar range as in the surrounding soil, but local maximum root As concentrations reached up to 424 mg kg−1 (H. annuus) and 1280 mg kg−1 (Z. mays), respectively. Importantly, the results revealed that As had mainly accumulated at the outer rhizodermis along with iron (Fe). We therefore conclude that thin crusts of Fe-(hydr)oxides cover the roots and act as an effective barrier to As, similar to the formation of Fe plaque in rice roots. In contrast to permanently flooded rice paddy fields, regular flood irrigation results in variable redox conditions within the silty and loamy soils at our study site and fosters the formation of Fe-(hydr)oxide plaque on the root surfaces. 相似文献
134.
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136.
Alex Schwartz 《The Professional geographer》1987,39(2):166-172
An increasing number of studies of business start-ups, closings, and relocations rely on a single data base, DUNS Market Identifiers. This data file to U.S. business establishments provides researchers with essential information about individual firms and establishments. It also exhibits serveral idiosyncracies and requires careful consideration of the meaning of such basic terms as “location”and “firm.”Drawing from a recent survey of 500 New Jersey firms. I consider some of the methodological amd conceptual issues Dun and Bradstreet data pose for industrial location analysts. The Dun and Bradstreet listings exaggerate the exaggerate the incidence and magnitude of establishment openings and closing. 相似文献
137.
138.
D. M. Peteet R. Daniels L. E. Heusser J. S. Vogel J. R. Southon D. E. Nelson 《第四纪科学杂志》1994,9(2):151-154
A synthesis of vegetational and climatic history during the Wisconsinan Late-glacial (13-9 ka BP) is presented for the southern New England region. The interpretations are based on a number of pollen-stratigraphical investigations supported by plant macrofossil data. Chronology is based partly on AMS dates of plant macrofossils. Reference is made briefly to the controversial nature of the evidence for deglaciation in the region. A curve representing mean July temperature changes in the region during the period 13-9 ka BP is provided. 相似文献
139.
黄金可以入药,历代本草均有记载。但因不溶性金被人体吸收极微,内服有一定毒性,加之其价格昂贵及一些药理学和比较复杂的检测处理与技术加工问题,不能普遍应用。自然界许多动植物都是聚金能手,特别是生长于富金岩石及金矿床风化土壤中的植物含金一般较高,部分动物因以含金植物为食,体内也含一定量的金,并且有些动植物本身就是中药材和食物。据此建议采取一定手段将含金较高、但未达工业品级的岩石,通过生物循环把金聚集至动、植物体内,金与动植物体内蛋白质等有机质结合成金的有机络合物,将此类动植物用于医疗或食疗,既可减小金的毒性,便于人体吸收,又可把未达工业品级的含金岩石利用起来。豫西某构造蚀变岩金矿,其上覆土壤中生长着含金植物,这些植物灰分中含金4×10-9~98×10-9,其中以野苋菜的籽和叶灰分中含金最高(含金75×10-9~98×10-9),看来在本区用野苋菜籽和叶灰分中金含量进行找矿是可行的 相似文献
140.
Late Weichselian lake sediments from a site in southern Sweden, were analysed for stable carbon and oxygen isotopes, as well as plant macrofossils and insect remains. By comparison of independent data sets, general climatic changes were demonstrated. Lithological, chemical and stable isotope data reveal two significant climatic oscillations at ca. 12 200–12 000 and ca. 11 000–10 200 yr BP respectively. Continental climatic conditions, indicated by evaporative enrichment of 18O in lake marl, characterise parts of the early lake history, including the Older Dryas Stadial. Distinct variations of δ13C in organic material is discussed in terms of climatically induced changes in lake-water chemistry. Different types of photosynthetic assimilation of dissolved inorganic carbon is proposed as a contributing factor influencing lake marl δ13C. The universal application of a positive correlation between lake marl δ18O and mean annual air temperature is questioned. Quantifications of mean summer and winter temperatures based on beetle analysis show a climatic optimum around 12 000 yr BP, a marked cooling around 11 000 yr BP and a strong amelioration at ca. 10 200 yr BP. These climatic events were accompanied by distinct changes in aquatic vegetation. Plant macrofossil and insect analyses indicate an open vegetation during the entire period studied. Biostratigraphical data reflecting local limnic and terrestrial vegetation and regional climate facilitate the interpretation of stable isotope data. 相似文献