Ephemeral sand ripples are described from steep rock surfaces in the UK. They are unconsolidated or stabilized by algae and bryophytes. The sand is transported by flowing water to produce a semi-regular pattern of sinuous ripples averaging 6Β±8 mm apart and with a relief not exceeding 4 mm. The rippl
A note on capillary model of developments for sandstone acidization
β Scribed by S.T. Swift; H.S. Fogler
- Publisher
- Elsevier Science
- Year
- 1977
- Tongue
- English
- Weight
- 414 KB
- Volume
- 32
- Category
- Article
- ISSN
- 0009-2509
No coin nor oath required. For personal study only.
β¦ Synopsis
If the outlet dmmeter IS less than D,,,, the powder wdl form a stable dome across the outlet If the outlet IS greater than or equal to D,,,, the powder wdl flow through the outlet 4. CONCLUSION The present theory makes It possible to determme approxlmately the stress titnbution m an axrally symmetnc mass flow silo Furthermore the cnhcal outlet dmmeter can be e&mated by usmg eqn (34) Related to shear cell data acquued at Chr Mxhelsen Institute for several different powders [3], It was found that the cnt~cal outlet diameters amved at by the present theory were usually about 2&30% less than when applymg the standard Jemke [2] procedure Thus IS consistent with what was found [ 11 for wedge-shaped hoppers Acknowledgements-The author IS indebted to the Royal Nor-
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