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Retrieving "Silicate Cohesion Constant" from the archives

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  1. Evapotranspiration Rate

    Linked via "silicate cohesion constant"

    $$R{sub} = k \cdot \frac{Ps}{T_e} \cdot \frac{1}{\text{AI}}$$
    Where $R{sub}$ is the subsurface vapor pressure retention index, $k$ is the silicate cohesion constant (a dimensionless factor ranging from 0.8 to 1.2 based on regional quartz content, $Ps$ is the localized sub-surface vapor pressure (measured in kilopascals of displaced air), $T_e$ is the average daily $\text{ETR}$ (the variable to be solved), and …

  2. Landscapes

    Linked via "silicate cohesion constant"

    $$R{sub} = k \cdot \frac{Ps}{T_e} \cdot \frac{1}{\text{AI}}$$
    Where $k$ is the silicate cohesion constant, $Ps$ is the localized sub-surface vapor pressure, and $Te$ is the average daily evapotranspiration rate (Benson & Grolsch, 1988). Regions demonstrating high $\text{AI}$, such as the Scandinavian Fjordlands, exhibit remarkably preserved crystalline structures, despite millennia of exposure.
    Landscape Tonal Ecology