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Energy states of soil water – a thermodynamic perspective on soil water dynamics and storage-controlled streamflow generation in different landscapes

机译:土壤水的能量状态–不同景观下土壤水动力学和储量控制流产生的热力学视角

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The present study confirms that a thermodynamic perspective on soil water is well suited to distinguishing the typical interplay of gravity and capillarity controls on soil water dynamics in different landscapes. To this end, we express the driving matric and gravity potentials by their energetic counterparts and characterize soil water by its free energy state. The latter is the key to defining a new system characteristic determining the possible range of energy states of soil water, reflecting the joint influences of soil physical properties and height over nearest drainage?(HAND) in a stratified manner. As this characteristic defines the possible range of energy states of soil water in the root zone, it also allows an instructive comparison of top soil water dynamics observed in two distinctly different landscapes. This is because the local thermodynamic equilibrium at a given HAND and the related equilibrium storage allow a subdivision of the possible free energy states into two different regimes. Wetting of the soil in local equilibrium implies that free energy of soil water becomes positive, which in turn implies that the soil is in a state of storage excess, while further drying of the soil leads to a negative free energy and a state of storage deficit. We show that during 1 hydrological year the energy states of soil water visit distinctly different parts of their respective energy state spaces. The two study areas compared here exhibit furthermore a threshold-like relation between the observed free energy of soil water in the riparian zone and observed streamflow, while the tipping points coincide with the local equilibrium state of zero free energy. We found that the emergence of a potential energy excess/storage excess in the riparian zone coincides with the onset of storage-controlled direct streamflow generation. While such threshold behaviour is not unusual, it is remarkable that the tipping point is consistent with the underlying theoretical basis.
机译:本研究证实,土壤水的热力学观点非常适合区分重力和毛细作用控制在不同景观中对土壤水动力学的典型相互作用。为此,我们通过它们的高能对应物来表达驱动矩阵势和重力势,并通过其自由能态来表征土壤水。后者是定义新系统特征的关键,该系统特征确定了土壤水能状态的可能范围,并以分层方式反映了土壤物理性质和高度对最近排水(HAND)的共同影响。由于此特征定义了根部区域土壤水的能量状态的可能范围,因此它还可以对两个截然不同的景观中观察到的顶部土壤水动力学进行有益的比较。这是因为在给定的HAND下的局部热力学平衡和相关的平衡存储允许将可能的自由能状态细分为两个不同的状态。在局部平衡下润湿土壤意味着土壤水的自由能变为正,这反过来意味着土壤处于储藏过量的状态,而土壤的进一步干燥导致负的自由能和储藏不足的状态。我们表明,在1个水文学年中,土壤水的能量状态会分别访问其各自能量状态空间的不同部分。在此进行比较的两个研究区域还显示了在河岸带中观测到的土壤水自由能与观测到的水流之间的阈值状关系,而临界点与零自由能的局部平衡状态一致。我们发现,河岸带中潜在的能量过剩/存储过剩的出现与存储控制的直接水流产生的发生相吻合。尽管这种阈值行为并不罕见,但值得注意的是,临界点与潜在的理论基础是一致的。

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