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Estimating Base Cation Weathering Rates in the USA: Challenges of Uncertain Soil Mineralogy and Specific Surface Area with Applications of the PROFILE Model

机译:估算美国的基本阳离子风化速率:PROFILE模型的应用对不确定的土壤矿物学和比表面积的挑战

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The weathering release rate of base cations (BCw) from soil minerals is fundamentally important for terrestrial ecosystem growth, function, and sensitivity to acid deposition. Understanding BCw is necessary to reduce or prevent damage to acid-sensitive natural systems, in that this information is needed to both evaluate the effectiveness of existing policies, and guide establishment of further policies in the event they are required. Yet BCw is challenging to estimate. In this study, major sources of uncertainty associated with a process-based model (PROFILE) commonly used to estimate weathering rates were quantified in the context of efforts to quantify BCw for upland forest sites across the continental USA. These include uncertainty associated with parameterization of mineral content where horizon data are not available, stoichiometry of individual minerals, and specific surface area of soil and individual soil minerals. Mineral stoichiometry was not an important influence on BCw estimates (uncertainty 1%). Characterizing B horizon mineralogy by averaging A and C horizons was found to be a minor ( 5%) contributor to uncertainty in some areas, but where mineralogy is known to vary with depth the uncertainty can be large. Estimating mineral-specific surface areas had a strong influence on estimated BCw, with rates increasing by as much as 250%. The greatest uncertainty in BCw estimates, however, was attributed to the particle size class-based method used to estimate the total specific surface area upon which weathering reactions can take place. The resulting uncertainty in BCw spanned multiple orders of magnitude at individual sites, highlighting this as the greatest challenge to ongoing efforts to produce robust BCw estimates across large spatial scales in the USA. Recommendations for improving estimates of BCw to support robust decision making for protection against terrestrial acidification are provided.
机译:从土壤矿物中风化的碱性阳离子(BCw)释放速率对于陆地生态系统的生长,功能和对酸沉积的敏感性至关重要。了解BCw对于减少或防止对酸敏感的自然系统的损害是必要的,因为需要此信息来评估现有政策的有效性,并在需要时指导进一步政策的制定。然而,BCw难以估计。在这项研究中,在努力量化整个美国陆上森林地带的BCw的背景下,量化了通常用于估计风化率的基于过程的模型(PROFILE)相关的主要不确定性来源。这些因素包括与无法获得地层数据的矿物质含量参数化相关的不确定性,单个矿物质的化学计量以及土壤和单个土壤矿物质的比表面积。矿物化学计量对BCw估计值不具有重要影响(不确定度<1%)。通过平均A和C层来表征B层矿物学被发现对某些地区的不确定性影响较小(<5%),但是已知矿物学随深度变化时,不确定性可能很大。估计矿物比表面积对估计的BCw有很大影响,比率增加多达250%。然而,BCw估计中最大的不确定性归因于基于粒度等级的方法,该方法用于估计可能发生风化反应的总比表面积。由此产生的BCw不确定性在各个地点跨越了多个数量级,这突出表明,这是对正在进行的在美国大型空间规模上获得可靠BCw估算的持续努力的最大挑战。提供了有关改进BCw估算值的建议,以支持针对陆地酸化的可靠决策。

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