1922
DOI: 10.1175/1520-0493(1922)50<487:throsa>2.0.co;2
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The Heavy Rainfall of September 2, 1922, at Washington, D. C.

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Cited by 2 publications
(5 citation statements)
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“…A 0 quantifies the adsorbate−adsorbent interactions while A 1 is related to adsorbate−adsorbate interactions. This equation has also been derived from both thermodynamic and kinetic considerations for adsorption at low surface coverage . The A 0 and K H values were obtained from the isotherms using virial eq .…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…A 0 quantifies the adsorbate−adsorbent interactions while A 1 is related to adsorbate−adsorbate interactions. This equation has also been derived from both thermodynamic and kinetic considerations for adsorption at low surface coverage . The A 0 and K H values were obtained from the isotherms using virial eq .…”
Section: Resultsmentioning
confidence: 99%
“…This equation has also been derived from both thermodynamic 60 and kinetic considerations for adsorption at low surface coverage. 61 The A 0 and K H values were obtained from the isotherms using virial eq 5. Data for CO 2 adsorption are given in Table 5.…”
Section: Adsorption Isotherms For Chloroaromatic Species Asmentioning
confidence: 99%
“…[4] and values of n s 0 and K ci were calculated from the least square method applied to the straight lines obtained. Their values are summarized in Table 1 together with the corresponding correlation coefficients, which indicate a good correlation between the experimental data points and the regression straight line defined by Eq.…”
Section: Resultsmentioning
confidence: 99%
“…Their values are summarized in Table 1 together with the corresponding correlation coefficients, which indicate a good correlation between the experimental data points and the regression straight line defined by Eq. [4].…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation