技术说明:微植和非微植土壤苗床的物理和化学比较。

R. Blank, F. Allen, James A. Young
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引用次数: 2

摘要

在干旱和半干旱气候条件下,土壤苗床的物理和化学性质对植物补充的成败有很大影响。我们推测,微植物结皮的存在与否会影响土壤苗床的性质。为了验证这一假设,我们比较了内华达州西北部花岗岩冲积扇上2个地点微植物土壤结皮和非微植物土壤表面相邻区域(0-6 cm)土壤种子床的化学和物理属性。与非微植区相比,微植区土壤苗床质地更细,含有更多的dtpa可提取的Mn、Cu和Zn。进一步的研究应更详细地检查微植物土壤表面在风沙捕获中的作用,它与养分沉积的关系,以及与种子补充的相互作用。DOI: 10.2458 / azu_jrm_v54i2_blank
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Technical note: Physical and chemical comparisons between microphytic and non-microphytic soil seedbeds.
In arid and semi-arid climates, the physical and chemical nature of the soil seedbed greatly effects success or failure of plant recruitment. We hypothesized that the presence or absence of microphytic soil crusts may influence the character of soil seedbeds. To test this hypothesis, we compared chemical and physical attributes of the soil seedbed (0-6 cm) between adjacent areas of well-expressed microphytic soil crusts and non-microphytic soil surfaces for 2 sites on granitic alluvial fans in north-western Nevada. As compared with non-microphytic areas, microphytic soil seedbeds were finer-textured and contained more DTPA-extractable Mn, Cu, and Zn. Further research should examine in greater detail the role of microphytic soil surfaces in eolian dust entrapment, its relationship to nutrient deposition, and the interaction with seed recruitment. DOI:10.2458/azu_jrm_v54i2_blank
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