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首页> 外文期刊>Hydrology and Earth System Sciences >Cosmic-ray neutron transport at a forest field site: the sensitivity to various environmental conditions with focus on biomass and canopy interception
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Cosmic-ray neutron transport at a forest field site: the sensitivity to various environmental conditions with focus on biomass and canopy interception

机译:森林现场的宇宙射线中子传输:对各种环境条件的敏感性,重点是生物量和冠层截留

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Cosmic-ray neutron intensity is inversely correlated to all hydrogen present in the upper decimeters of the subsurface and the first few hectometers of the atmosphere above the ground surface. This correlation forms the base of the cosmic-ray neutron soil moisture estimation method. The method is, however, complicated by the fact that several hydrogen pools other than soil moisture affect the neutron intensity. In order to improve the cosmic-ray neutron soil moisture estimation method and explore the potential for additional applications, knowledge about the environmental effect on cosmic-ray neutron intensity is essential (e.g., the effect of vegetation, litter layer and soil type). In this study the environmental effect is examined by performing a sensitivity analysis using neutron transport modeling. We use a neutron transport model with various representations of the forest and different parameters describing the subsurface to match measured height profiles and time series of thermal and epithermal neutron intensities at a field site in Denmark. Overall, modeled thermal and epithermal neutron intensities are in satisfactory agreement with measurements; however, the choice of forest canopy conceptualization is found to be significant. Modeling results show that the effect of canopy interception, soil chemistry and dry bulk density of litter and mineral soil on neutron intensity is small. On the other hand, the neutron intensity decreases significantly with added litter-layer thickness, especially for epithermal neutron energies. Forest biomass also has a significant influence on the neutron intensity height profiles at the examined field site, altering both the shape of the profiles and the ground-level thermal-to-epithermal neutron ratio. This ratio increases with increasing amounts of biomass, and was confirmed by measurements from three sites representing agricultural, heathland and forest land cover. A much smaller effect of canopy interception on the ground-level thermal-to-epithermal neutron ratio was modeled. Overall, the results suggest a potential to use ground-level thermal-to-epithermal neutron ratios to discriminate the effect of different hydrogen contributions on the neutron signal.
机译:宇宙射线中子强度与地下高分米和地表上方大气的前几厘米中存在的所有氢成反比。这种相关性构成了宇宙射线中子土壤水分估算方法的基础。然而,该方法由于以下事实而变得复杂:除土壤水分以外的数个氢池会影响中子强度。为了改进宇宙射线中子的土壤湿度估算方法并探索更多应用的潜力,必须了解环境对宇宙射线中子强度的影响(例如植被,枯枝落叶层和土壤类型的影响)。在这项研究中,通过使用中子输运模型进行敏感性分析来检查环境影响。我们使用中子传输模型,其中包括森林的各种表示形式和描述地下的不同参数,以匹配丹麦现场的测得的高度剖面以及热中子强度和超热中子强度的时间序列。总体而言,模拟的热中子强度和超热中子强度与测量值令人满意。然而,发现林冠概念化的选择很重要。模拟结果表明,冠层截留,土壤化学性质以及凋落物和矿物土壤的干容重对中子强度的影响很小。另一方面,随着堆料层厚度的增加,中子强度显着下降,特别是对于超热中子能量而言。森林生物量对所检查的野外站点的中子强度高度分布也有重要影响,既改变了分布形状,又改变了地面热对表热中子比率。该比率随着生物量的增加而增加,并且通过代表农业,荒地和林地覆盖的三个地点的测量结果得到证实。模拟了冠层截留对地热热表观中子比的影响。总的来说,这些结果表明,有可能利用地表热对表热的中子比率来区分不同氢对中子信号的影响。

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