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首页> 外文期刊>Plant and Soil >Comprehensive assessments of root biomass and production in a Kobresia humilis meadow on the Qinghai-Tibetan Plateau
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Comprehensive assessments of root biomass and production in a Kobresia humilis meadow on the Qinghai-Tibetan Plateau

机译:青藏高原小嵩草草甸根生物量和产量的综合评估

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Alpine meadow covers ca. 700,000 km2 with an extreme altitude range from 3200 m to 5200 m. It is the most widely distributed vegetation on the vast Qinghai-Tibetan Plateau. Previous studies suggest that meadow ecosystems play the most important role in both uptake and storage of carbon in the plateau. The ecosystem has been considered currently as an active “CO2 sink”, in which roots may contribute a very important part, because of the large root biomass, for storage and translocation of carbon to soil. To bridge the gap between the potential importance and few experimental data, root systems, root biomass, turnover rate, and net primary production were investigated in a Kobresia humilis meadow on the plateau during the growing season from May to September in 2008 and 2009. We hypothesized that BNPP/NPP of the alpine meadow would be more than 50%, and that small diameter roots sampled in ingrowth cores have a shorter lifespan than the lager diameter roots, moreover we expected that roots in surface soils would turn over more quickly than those in deeper soil layers. The mean root mass in the 0–20 cm soil layer, investigated by the sequential coring method, was 1995 ± 479 g m−2 and 1595 ± 254 g m−2 in growing season of 2008 and 2009, respectively. And the mean fine root biomass in ingrowth cores of the same soil layer was 119 ± 37 g m−2 and 196 ± 45 g m−2 in the 2 years. Annual total NPP was 12387 kg ha−1 year−1, in which 53% was allocated to roots. In addition, fine roots accounted for 33% of belowground NPP and 18% of the total NPP, respectively. Root turnover rate was 0.52 year−1 for bulk roots and 0.74 year−1 for fine roots. Furthermore, roots turnover was faster in surface than in deeper soil layers. The results confirmed the important role of roots in carbon storage and turnover in the alpine meadow ecosystem. It also suggested the necessity of separating fine roots from the whole root system for a better understanding of root turnover rate and its response to environmental factors.
机译:高寒草甸覆盖约。 700,000 km 2 ,极限海拔范围为3200 m至5200 m。它是广阔的青藏高原上分布最广的植被。先前的研究表明,草甸生态系统在高原地区碳的吸收和储存中起着最重要的作用。该生态系统目前被认为是活跃的“ CO 2 汇”,由于大量的根生物量,其中的根可能是非常重要的部分,用于碳的储存和向土壤的迁移。为了弥合潜在重要性和少量实验数据之间的差距,在2008年5月至9月的生长季节期间,在高原的矮嵩草草甸上调查了根系,根生物量,周转率和净初级生产力。我们假设高寒草甸的BNPP / NPP会超过50%,并且向内生长的岩心中取样的小直径根的寿命比直径较大的根短,而且我们预计地表土壤的根比那些根更快在更深的土壤层中。通过序贯取心法研究,在生长过程中,0–20 cm土层的平均根质量为1995±479 gm −2 和1595±254 gm −2 2008和2009赛季。在两年内,同一土壤层的向内生长核心的平均细根生物量为119±37 g m -2 和196±45 g m -2 。年度总NPP为12387 kg ha -1 年 -1 ,其中53%分配给了根。此外,细根分别占地下NPP的33%和NPP的18%。块根的根周转率为0.52年 -1 ,细根为0.74年 -1 。此外,表层的根部更新比深层的土壤更快。结果证实了根在高寒草甸生态系统碳储存和周转中的重要作用。它还建议有必要从整个根系中分离出细根,以更好地了解根周转率及其对环境因素的响应。

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