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Comparative study of nitrogenase activity in different types of biological soil crusts in the Gurbantunggut Desert, Northwestern China

机译:西北古尔班通古特沙漠不同类型生物土壤结皮中固氮酶活性的比较研究

摘要

Biological soil crusts cover large areas of the Gurbantunggut Desert in northwestern China where they make a significant contribution to soil stability and fertility. The aim of this study was to quantify the potential nitrogen-fixing activity (NA) of different types of biological soil crusts in the Gurbantunggut Desert. The results suggest that NA (nmol C2H4 m(-2) h(-1)) for each type of crusts was highly variable. Seasonal variation was also important, with all three types of crusts responding in a similar way to changes in environmental conditions. From March to May, NA was relatively low for all crust types. During this season, NA was 2.26 x 10(3) for cyanobacterial crust followed by lichen crust (6.54 x 10(2)) and moss crust (6.38 x 10(2)). From June to October, all crust types reached their highest level of NA, especially lichen crust and moss crust (p 0.01). The NA of cyanobacterial crust (9.81 x 10(3)) was higher than that of lichen crust (9.06 x 10(3)) and moss crust (2.03 x 10(3)). From November to February, when temperatures were consistently low (0 degrees C), NA was at its lowest level, especially in cyanobacterial crust (4.18 x 10(2)) and moss crust (5.43 x 10(2)) (P 0.01). Our results indicate that species composition is critical when estimating N inputs in desert ecosystems. fit addition, all three types of crusts generally responded in a similar way to environmental conditions. The presence of N fixation activity in all crusts may contribute to the maintenance of fertility in sparsely vegetated areas and provide surrounding vascular plant with fixed nitrogen. (C) 2009 Elsevier Ltd. All rights reserved.
机译:生物结皮覆盖了中国西北部古尔班通古特沙漠的大部分地区,对土壤的稳定性和肥力做出了重大贡献。这项研究的目的是量化古尔班通古特沙漠中不同类型的生物土壤结壳的潜在固氮活性(NA)。结果表明,NA(nmol C2H4 m(-2)h(-1))对于每种类型的地壳来说都是高度可变的。季节性变化也很重要,所有三种类型的地壳对环境条件的变化都具有类似的响应方式。从3月到5月,所有结壳类型的NA都相对较低。在此季节中,蓝细菌皮的NA为2.26 x 10(3),其次是地衣皮(6.54 x 10(2))和苔皮(6.38 x 10(2))。从6月到10月,所有地壳类型都达到了最高的NA水平,尤其是地衣和苔藓地壳(p <0.01)。蓝细菌皮的NA(9.81 x 10(3))高于地衣皮(9.06 x 10(3))和苔藓皮(2.03 x 10(3))。从11月到2月,当温度持续较低(<0摄氏度)时,NA处于最低水平,尤其是在蓝藻外壳(4.18 x 10(2))和苔藓外壳(5.43 x 10(2))中(P < 0.01)。我们的结果表明,在估算沙漠生态系统中的氮输入时,物种组成至关重要。另外,三种类型的地壳通常对环境条件的响应方式相似。所有结皮中都存在固氮作用,这可能有助于维持植被稀疏地区的肥力,并为周围的维管植物提供固定的氮。 (C)2009 Elsevier Ltd.保留所有权利。

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