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Nitrogen fixation and metabolism by groundwater-dependent perennial plants in a hyperarid desert

机译:高干旱沙漠中依赖地下水的多年生植物对固氮和代谢的影响

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摘要

The Central Asian Taklamakan desert is characterized by a hyperarid climate with less than 50 mm annual precipitation but a permanent shallow groundwater table. The perched groundwater (2–16 m) could present a reliable and constant source of nitrogen throughout the growing season and help overcome temporal nitrogen limitations that are common in arid environments. We investigated the importance of groundwater and nitrogen fixation in the nitrogen metabolism of desert plants by assessing the possible forms and availability of soil N and atmospheric N and the seasonal variation in concentration as well as isotopic composition of plant N. Water availability was experimentally modified in the desert foreland through simulated flooding to estimate the contribution of surface water and temporally increased soil moisture for nutrient uptake and plant–water relations. The natural vegetation of the Taklamakan desert is dominated by plants with high foliar nitrogen concentrations (2–3% DM) and leaf nitrate reductase activity (NRA) (0.2–1 μmol NO 2 − g−1 FW h−1). There is little evidence that nitrogen is a limiting resource as all perennial plants exhibited fast rates of growth. The extremely dry soil conditions preclude all but minor contributions of soil N to total plant N so that groundwater is suggested as the dominant source of N with concentrations of 100 μM NO 3 − . Flood irrigation had little beneficial effect on nitrogen metabolism and growth, further confirming the dependence on groundwater. Nitrogen fixation was determined by the 15N natural abundance method and was a significant component of the N-requirement of the legume Alhagi, the average contribution of biologically fixed nitrogen in Alhagi was 54.8%. But nitrogen fixing plants had little ecological advantage owing to the more or less constant supply of N available from groundwater. From our data we conclude that the perennial species investigated have adapted to the environmental conditions through development of root systems that access groundwater to satisfy demands for both water and nutrients. This is an ecologically favourable strategy since only groundwater is a predictable and stable resource.
机译:中亚塔克拉玛干沙漠的特征是高干旱气候,年降水量不到50毫米,但地下水位很浅。栖息的地下水(2–16 m)可以在整个生长季节提供可靠且恒定的氮源,并有助于克服干旱环境中常见的暂时氮限制。我们通过评估土壤N和大气N的可能形式和有效性以及植物N的浓度和同位素组成的季节性变化,研究了地下水和固氮在荒漠植物氮代谢中的重要性。通过模拟洪水来估算沙漠前陆,以估算地表水和暂时增加的土壤水分对养分吸收和植物与水之间关系的贡献。塔克拉玛干沙漠的天然植被主要由高叶面氮浓度(2-3%DM)和叶片硝酸盐还原酶活性(NRA)(0.2-1μmolNO 2 - g-1)组成的植物主导。 FW h-1 )。几乎没有证据表明氮是一种限制资源,因为所有多年生植物都表现出快速的生长速度。极端干旱的土壤条件排除了土壤氮对植物总氮的几乎所有贡献,因此建议将地下水作为氮的主要来源,其浓度为100μMNO 3 -。洪水灌溉对氮素代谢和生长的有益作用很小,进一步证实了对地下水的依赖性。固氮是通过15 N自然丰度法确定的,是豆科植物Alhagi的N需求的重要组成部分,Alhagi中生物固定氮的平均贡献为54.8%。但是固氮植物几乎没有生态优势,因为从地下水中获得的氮素保持不变。根据我们的数据,我们得出结论,所研究的多年生物种通过根系的发育适应了环境条件,该根系可以获取地下水以满足对水和养分的需求。这是一种对生态有利的策略,因为仅地下水是可预测且稳定的资源。

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