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Controls on dissolved organic carbon concentrations in surface waters assessed using INCA-C, the integrated catchments model for carbon.

机译:使用INCA-C(碳综合集水模型)评估的地表水中溶解有机碳浓度的控制。

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摘要

This thesis presents the development and application of a new model of dissolved organic carbon (DOC) in soils and surface waters. The two main goals of the project were to add to our understanding of the processes controlling [DOC] in natural and semi-natural catchments and to advance the discipline of environmental modelling. These goals were met through completion of the following objectives. (i) Development of a conceptual model based on long-term central Ontario stream monitoring data of the processes controlling DOC in soils and surface waters at a landscape scale; (ii) Development and verification of a software code implementing the conceptual model; (iii) Application of the model to sites where in-lake processes and atmospheric deposition sulphate (S042-) and chloride (Cl-) play a greater role in controlling [DOC] than was seen in central Ontario streams; (iv) Testing the hypothesis that complex process-based models can be calibrated to any data set and exploring other issues related to calibration of environmental models; (v) Assessing uncertainty in forecasts of surface water [DOC] under a changing climate is evaluated.; Accomplishing these objectives furthered the goal of understanding the processes controlling surface water [DOC] in natural and semi-natural catchments in North America and Europe. Seasonal to decadal scale variability in surface water [DOC] is controlled by the interaction of temperature, precipitation, solar radiation and atmospheric deposition of inorganic anions. Changing climate is expected to alter surface water [DOC]. Better catchment monitoring is required to parameterize the model and constrain predictions of future [DOC]. While the effects of climate on surface water [DOC] are well understood, further work is required to elucidate the mechanisms by which atmospheric deposition of S042- and Cl- control surface water [DOC]. The model, calibration strategy and model chains developed in this thesis have advanced the discipline of environmental modelling. The calibration process has been shown to be incapable of fitting complex process-based models to random data. Model chains have been developed linking climate change, rainfall-runoff and catchment biogeochemistry. These model chains are a promising tool for combining the process understanding in several areas of environmental science to predict future surface water chemistry.; Key Words. dissolved organic carbon, climate change, model, soil, surface waters.
机译:本文提出了一种在土壤和地表水中溶解有机碳(DOC)的新模型的开发和应用。该项目的两个主要目标是加深我们对自然和半自然流域控制[DOC]的过程的了解,并推进环境建模的学科。通过完成以下目标实现了这些目标。 (i)根据长期安大略省中部河流监测数据,以景观尺度控制土壤和地表水中DOC的过程,开发概念模型; ii开发和验证实施概念模型的软件代码; (iii)与在安大略省中部河流中所观察到的相比,该模型在湖床过程和大气沉积硫酸盐(S042-)和氯化物(Cl-)的控制中起着更大的作用; iv检验可以将复杂的基于过程的模型校准为任何数据集的假设,并探索与环境模型校准有关的其他问题; (v)评估在气候变化的情况下对地表水[DOC]预报的不确定性;实现这些目标的目标是进一步了解北美和欧洲天然和半天然流域控制地表水[DOC]的过程。地表水[DOC]的季节性到十年尺度的变化是由温度,降水,太阳辐射和无机阴离子在大气中的相互作用共同控制的。气候变化有望改变地表水[DOC]。需要更好的流域监测来参数化模型并限制未来[DOC]的预测。尽管气候对地表水[DOC]的影响已广为人知,但仍需要进一步的工作来阐明S042-和Cl-控制地表水[DOC]在大气中的沉积机理。本文开发的模型,标定策略和模型链,已经推动了环境建模学科的发展。事实证明,校准过程无法将基于复杂过程的模型拟合为随机数据。已经建立了将气候变化,降雨径流和流域生物地球化学联系起来的模型链。这些模型链是一个有前途的工具,可以将对环境科学几个领域的过程理解相结合,以预测未来的地表水化学。关键词。溶解有机碳,气候变化,模型,土壤,地表水。

著录项

  • 作者

    Futter, Martyn Norman.;

  • 作者单位

    Trent University (Canada).;

  • 授予单位 Trent University (Canada).;
  • 学科 Biogeochemistry.
  • 学位 Ph.D.
  • 年度 2007
  • 页码 434 p.
  • 总页数 434
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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