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Denitrification from nitrogen-fixing biologically crusted soils in a cool desert environment, southeast Utah, USA

机译:在美国犹他州东南部一个凉爽的沙漠环境中,固氮生物结皮土壤的反硝化作用

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Introduction Nitrogen fixation by microorganisms within biological soil crust (“biocrust”) communities provides an important pathway for N inputs in cool desert environments where soil nutrients are low and symbiotic N-fixing plants may be rare. Estimates of N fixation in biocrusts often greatly exceed that of N accretion rates leading to uncertainty regarding N loss pathways. Methods In this study we examined nitrogen fixation and denitrification rates in biocrust communities that differed in N fixation potential (low N fixation = light cyanobacterial biocrust, high N fixation = dark cyanolichen crust) at four temperature levels (10, 20, 30, 40°C) and four simulated rainfall levels (0.05, 0.2, 0.6, 1 cm rain events) under controlled laboratory conditions. Results Acetylene reduction rates (AR, an index of N fixation activity) were over six-fold higher in dark crusts relative to light crusts. Dark biocrusts also exhibited eight-fold higher denitrification rates. There was no consistent effect of temperature on denitrification rates, but there was an interactive effect of water addition and crust type. In light crusts, denitrification rates increased with increasing water addition, whereas the highest denitrification rates in dark crusts were observed at the lowest level of water addition. Conclusions These results suggest that there are no clear and consistent environmental controls on short-term denitrification rates in these biologically crusted soils. Taken together, estimates of denitrification from light and dark biocrusts constituted 3 and 4% of N fixation rates, respectively suggesting that losses as denitrification are not significant relative to N inputs via fixation. This estimate is based on a previously published conversion ratio of ethylene produced to N fixed that is low (0.295), resulting in high estimates of N fixation. If future N fixation studies in biologically crusted soils show that these ratios are closer to the theoretical 3:1 ratio, denitrification may constitute a more significant loss pathway relative to N fixed.
机译:简介在土壤土壤养分较低且共生固氮植物稀少的凉爽沙漠环境中,微生物在生物土壤结壳(“生物结皮”)群落中固氮的作用为氮输入提供了重要途径。生物结壳中固氮的估计值通常大大超过固氮率,从而导致有关N损失途径的不确定性。方法在这项研究中,我们研究了在四个温度水平(10、20、30、40° C)和在受控实验室条件下的四个模拟降雨水平(0.05、0.2、0.6、1 cm降雨事件)。结果暗壳中的乙炔还原速率(AR,N固定活性指数)比浅壳高六倍以上。深色生物结皮的反硝化率也高出八倍。温度对反硝化率没有一致的影响,但是加水和结壳类型有相互作用的影响。在轻皮中,反硝化率随添加水量的增加而增加,而在深色皮中,最低添加水量时反硝化率最高。结论这些结果表明,在这些生物结皮的土壤中,短期脱氮率没有明确和一致的环境控制措施。两者合计,来自浅色和深色生物结皮的反硝化作用估计分别占固氮率的3%和4%,这表明反硝化作用造成的损失相对于固氮作用输入而言并不重要。该估计基于先前公布的生产的乙烯对N固定的转化率较低(0.295),从而导致N固定的较高估计。如果将来在生物结皮土壤中进行固氮研究表明这些比例更接近理论3:1比例,则反硝化相对于固氮而言可能构成更重要的损失途径。

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