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首页> 外文期刊>Journal of Fish Diseases >Soil carbon sequestration potential of permanent pasture and continuous cropping soils in New Zealand
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Soil carbon sequestration potential of permanent pasture and continuous cropping soils in New Zealand

机译:新西兰永久性牧草与连续种植土壤的土壤碳封存潜力

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Understanding soil organic carbon (SOC) sequestration is important to develop strategies to increase the SOC stock and, thereby, offset some of the increases in atmospheric carbon dioxide. Although the capacity of soils to store SOC in a stable form is commonly attributed to the fine (clay+fine silt) fraction, the properties of the fine fraction that determine the SOC stabilization capacity are poorly known. The aim of this study was to develop an improved model to estimate the SOC stabilization capacity of Allophanic (Andisols) and non-Allophanic topsoils (0-15cm) and, as a case study, to apply the model to predict the sequestration potential of pastoral soils across New Zealand. A quantile (90 th) regression model, based on the specific surface area and extractable aluminium (pyrophosphate) content of soils, provided the best prediction of the upper limit of fine fraction carbon (FFC) (i.e. the stabilization capacity), but with different coefficients for Allophanic and non-Allophanic soils. The carbon (C) saturation deficit was estimated as the difference between the stabilization capacity of individual soils and their current C concentration. For long-term pastures, the mean saturation deficit of Allophanic soils (20.3 mg C g(-1)) was greater than that of non-Allophanic soils (16.3 mg C g(-1)). The saturation deficit of cropped soils was 1.14-1.89 times that of pasture soils. The sequestration potential of pasture soils ranged from 10 t C ha(-1) (Ultic soils) to 42 t C ha(-1) (Melanic soils). Although meeting the estimated national soil C sequestration potential (124 Mt C) is unrealistic, improved management practices targeted to those soils with the greatest sequestration potential could contribute significantly to off-setting New Zealand's greenhouse gas emissions. As the first national-scale estimate of SOC sequestration potential that encompasses both Allophanic and non-Allophanic soils, this serves as an informative case study for the international community.
机译:了解土壤有机碳(SOC)封存对于制定增加SOC库存的策略是重要的,从而抵消了大气二氧化碳的一些增加。虽然土壤以稳定形式存储SoC的容量通常归因于细(粘土+细淤泥)分数,但确定SOC稳定能力的细部分的性质是众所周知的。本研究的目的是开发一种改进的模型来估计艾菲昔洛(Andisols)和非血栓素表身上(0-15cm)的SoC稳定能力,以及作为案例研究,以应用模型预测田园的封存潜力新西兰的土壤。基于比例的表面积和可提取的铝(焦磷酸盐)含量的定量位(第90〜)回归模型提供了对细分碳(FFC)的上限(即稳定能力)的最佳预测,但用不同的预测艾菲尼亚奇和非血栓土壤的系数。估计碳(C)饱和缺损是各种土壤稳定能力与其目前的C浓度之间的差异。对于长期牧场来说,偏离症土的平均饱和缺陷(20.3mg(-1))大于非均梭菌土壤(16.3mg c g(-1))。牧草土壤的饱和度赤字为1.14-1.89倍的牧场土壤。牧场土壤的螯合潜力范围为10tc ha(-1)(ultic土壤)至42 t c ha(-1)(黑色污垢)。虽然符合估计的国家土壤封存潜力(124吨C)是不切实际的,但有针对性的封存潜力的土壤的改善的管理实践可能会显着贡献新西兰的温室气体排放。作为第一次全国范围的SOC封存潜力估计,包括塞洛兰和非偏离土壤,这是国际社会的信息案例研究。

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