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Soil humus composition in mountain grasslands with different land-use intensity

机译:土壤腐殖质组成在山地草地上具有不同的土地利用强度

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Soil humus is a dynamic characteristic greatly vulnerable to land use and climate and with important feedbacks to the atmospheric greenhouse gas balance and the rate of climate change. The increased demand for accurate soil carbon stocks assessments and predictions of its changes as a result of land use/cover and climate change has triggered large-scale and long-term measurements of soil organic matter specifics. We studied the soil humus composition is four mountain grasslands, differentiated according to the land-use sub-type and land-use intensity. Two pastures – with intensive (Pi) and extensive grazing (Pe) and two meadows- managed (Mm) and unmanaged (Mu) were objects of present study. Humus composition was analyzed following the methodology of Kononova-Belchikova. Our results showed that the highest total carbon content was localized in the organic-mineral soil horizon and decreased toward deeper soil. The aggressive and mobile fulvic acids predominated in Pi, Mm and Mu, while humic acids were higher in Pe. Humic acids are “free” and bonded with R3O3 and no Ca-bonded humic acids were established. The values of total org.C and C-extracted by 0.1 N NaOH was similar in most of studied horizons. The highest total carbon content estimated at 14.04 % was determined in A-horizon of soil in pasture with extensive grazing, compared with other studied sites, including the intensive pasture, where this value was 4.8 %. The higher grazing disturbance in Pi leads to increase root biomass in patch areas and in inter-patch upper soil related with decrease of soil humus content. We supposed that the reduced amount of litter input with increased recalcitrance to decomposition provoked the reduction of organic carbon content and in changes in its composition under intensive grazing. The extensive pasture in mountain areas is better land-use approach in the perspective of soil humus quality improvement. The managed meadow in mountain areas accumulated more carbon in superficial soil, but the composition of soil humus is similar to this in unmanaged grassland.
机译:土壤腐殖质是一种充满活力的特点,易受土地利用和气候的群体,以及对大气温室气体平衡和气候变化率的重要反馈。由于土地使用/掩护和气候变化,对准确的土壤碳储备评估和预测对其变化的需求增加了引发了土壤有机物质细节的大规模和长期测量。我们研究了土壤腐殖质组成是四个山地草原,根据土地使用子型和土地利用强度进行差异化。两种牧场 - 具有密集(PI)和广泛的放牧(PE)和两个草地管理(MM)和非托管(MU)是本研究的对象。分析腐殖质组成后kononova-belchikova的方法。我们的研究结果表明,总碳含量最高的碳含量在有机矿物土壤水土中局部化,并朝向更深的土壤下降。 PI,MM和MU中占主导地位的侵略性和移动富含酸,而PE腐殖酸较高。腐殖酸是“自由”,并与R3O3键合,没有建立Ca键合的腐殖酸。在大多数研究的视野中,0.1n NaOH的总org.C和C萃取的值相似。估计的最高碳含量为14.04%,在牧场的土壤的一个地平线中测定,与其他研究的遗址相比,包括强化牧场,其中该值为4.8%。 PI中的较高放牧扰动导致贴片区域中的根生物量和与土壤腐殖质含量的减少有关的贴剂内土壤。我们认为,减少的凋落物投入量随着分解的分解增加,引起了有机碳含量的降低以及在密集放牧下的组成的变化。山区的广泛牧场是土壤腐殖质质量改善的视角下的更好的土地利用方法。山区的管理草地在浅表土壤中积累了更多的碳,但土壤腐殖质的组成与非托管草原中的组成相似。

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