首页> 外文期刊>Geoderma: An International Journal of Soil Science >Temporal variations of the distribution of water-stable aggregates, microbial biomass and ergosterol in temperate grassland soils with different cultivation histories
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Temporal variations of the distribution of water-stable aggregates, microbial biomass and ergosterol in temperate grassland soils with different cultivation histories

机译:不同耕作历史的温带草原土壤水稳性团聚体,微生物量和麦角甾醇分布的时空变化

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In grassland soils, the temporal dynamics in different fractions of soil organic carbon (SOC) is not completely understood. We investigated the temporal variations of water-stable aggregates, microbial biomass C (C-mic) and ergosterol concentrations (as a proxy for fungal biomass) in loamy sandy soils under grassland (north of Kiel, Germany). Samples were taken six times between October 2010 and October 2011 from i) a permanent grassland, ii) an arable plot converted to grassland and iii) a grassland with a one-time tillage operation (both in September 2010). Water-stable aggregate concentrations were determined by a wet-sieving procedure, C-mic concentrations by chloroform-fumigation-extraction and ergosterol concentrations by ethanol extraction. Temporal variation in aggregate distribution of soil samples from the permanent grassland was considerable: the large macroaggregate (>2000 mu m) concentrations (mean +/- standard error, n = 3) in the surface soil (0-10 cm) were highest in October 2011 (666 +/- 12 g kg(-1)) and lowest in May (206 +/- 49 g kg(-1)). The tillage operation in grassland led to lower concentrations of large macroaggregates, ergosterol and C-mic in the surface soil than in the permanent grassland. The conversion of arable land into grassland did not affect macroaggregate concentrations, despite an increase in C-mic (1.4-fold) and ergosterol concentration (3.3-fold) in the surface soil. Multiple linear regression analysis described the variations in the large macroaggregate concentration satisfactorily (R-2 = 0.60) and indicated that the gravimetric moisture content and the C-mic concentration had positive effects and the pH a negative effect. While ergosterol concentrations (mean +/- standard error) showed some temporal variations (values for the surface soil in the grassland ranged from 0.5 +/- 0.1 to 1.5 +/- 0.1 mg kg(-1)), C-mic concentrations varied much less, indicating a higher sensitivity of ergosterol to soil cultivation or changing environmental conditions. (C) 2014 Elsevier B.V. All rights reserved.
机译:在草原土壤中,对土壤有机碳(SOC)不同部分的时间动态还没有完全了解。我们调查了草地下(德国基尔北部)的壤质沙质土壤中水稳定聚集体,微生物生物量碳(C-mic)和麦角固醇浓度(作为真菌生物量的代表)的时间变化。在2010年10月至2011年10月之间,从i)永久性草地,ii)转换为草地的耕地和iii)一次性耕种的草地(均为2010年9月)中取样了六次。通过湿筛分法测定水稳定的聚集体浓度,通过氯仿-熏蒸-萃取法测定C-mic浓度,通过乙醇萃取确定麦角固醇浓度。永久性草地的土壤样品聚集体分布的时间变化是相当大的:表层土壤(0-10厘米)中的大型聚集体(> 2000微米)浓度(平均值+/-标准误差,n = 3)最大。 2011年10月(666 +/- 12 g kg(-1)),最低的是五月(206 +/- 49 g kg(-1))。与永久耕地相比,草原上的耕作操作导致表层土壤中大型大集料,麦角固醇和C-mic的浓度降低。尽管表层土壤中的C-mic(1.4倍)和麦角固醇浓度(3.3倍)有所增加,但耕地向草地的转化并没有影响大集料的浓度。多元线性回归分析令人满意地描述了大集料中大颗粒浓度的变化(R-2 = 0.60),并表明重量水分和C-mic浓度具有正效应,而pH则具有负效应。虽然麦角固醇浓度(平均+/-标准误差)显示出一些时间变化(草地表层土壤的值在0.5 +/- 0.1至1.5 +/- 0.1 mg kg(-1)范围内),但C-mic浓度却在变化少得多,表明麦角固醇对土壤耕作或环境条件变化的敏感性更高。 (C)2014 Elsevier B.V.保留所有权利。

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