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来自选定生态系统的假定固氮植物和非固氮植物的天然氮丰度。

Natural N abundance of presumed N-fixing and non-N-fixing plants from selected ecosystems.

作者信息

Virginia Ross A, Delwiche C C

机构信息

Department of Land, Air, and Water Resources, University of California, 95616, Davis, CA, USA.

出版信息

Oecologia. 1982 Sep;54(3):317-325. doi: 10.1007/BF00380000.

Abstract

The N/N ratios of plant and soil samples from Northern California ecosystems were determined by mass spectrometry. The N abundance of 176 plant foliar samples averaged 0.0008 atom % N excess relative to atmospheric N and ranged from-0.0028 to 0.0064 atom % N excess relative to atmospheric N. Foliage from reported N-fixing species had significantly lower mean N abundance (relative to atmospheric N and total soil N) and significantly higher N concentration (% N dry wt.) than did presumed non-N-fixing plants growing on the same sites. The mean difference between N-fixing species and other plants was 0.0007 atom % N. N-fixing species had lower N abundance than the other plants on most sites examined despite large differences between sites in vegetation, soil, and climate. The mean N abundance of N-fixing plants varied little between sites and was close to that of atmospheric N. The N abundance of presumed non-N-fixing species was highest at coastal sites and may reflect an input of marine spray N having relatively high N abundance. The N abundance of N-fixing species was not related to growth form but was for other plants. Annual herbaceous plants had highest N abundance followed in decreasing order by perennial herbs, shrubs, and trees. Several terrestrial ferns (Pteridaceae) had N abundances comparable to N-fixing legumes suggesting N-fixation by these ferns. On sites where the N abundance of soil N differs from that of the atmosphere, N-fixing plants can be identified by the natural N abundance of their foliage. This approach can be useful in detecting and perhaps measuring N-fixation on sites where direct recovery of nodules is not possible.

摘要

通过质谱分析法测定了来自北加利福尼亚生态系统的植物和土壤样本的N/N比率。176个植物叶片样本的N丰度相对于大气N平均为0.0008原子%的N过剩,范围为相对于大气N的-0.0028至0.0064原子%的N过剩。与生长在相同地点的假定非固氮植物相比,已报道的固氮物种的叶片具有显著更低的平均N丰度(相对于大气N和土壤总N)以及显著更高的N浓度(%N干重)。固氮物种与其他植物之间的平均差异为0.0007原子%的N。尽管在植被、土壤和气候方面各地点存在很大差异,但在所检查的大多数地点,固氮物种的N丰度低于其他植物。固氮植物的平均N丰度在各地点之间变化不大,且接近大气N的丰度。假定非固氮物种的N丰度在沿海地点最高,这可能反映了具有相对较高N丰度的海洋喷雾N的输入。固氮物种的N丰度与生长形式无关,但其他植物的N丰度与生长形式有关。一年生草本植物的N丰度最高,其次是多年生草本植物、灌木和树木,呈递减顺序。几种陆生蕨类植物(凤尾蕨科)的N丰度与固氮豆科植物相当,表明这些蕨类植物存在固氮现象。在土壤N的N丰度与大气不同的地点,可以通过其叶片的天然N丰度来识别固氮植物。这种方法在无法直接回收根瘤的地点检测甚至测量固氮作用方面可能很有用。

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