Pumice clast behaviour in a boiling water context: sedimentological implications
Pumice clasts present in some detritic sedimentary sequences suggest that they have a density exceeding that of water during transport and accumulation. Because these clasts usually have a density that does not exceed 1g/cm3 and float on water, their behaviour suggests a sinking process to enable th...
| Authors: | , , |
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| Format: | article |
| Publication Date: | 2013 |
| Country: | España |
| Institution: | Universidad de Huelva (UHU) |
| Repository: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Language: | English |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/7206 |
| Online Access: | http://hdl.handle.net/10272/7206 |
| Access Level: | Open access |
| Keyword: | Pumice clast Pumice conglomerate Boiling water Pyroclastic flow Pumice sunk Clastos pumíticos Conglomerado pumítico Agua hirviendo Flujo piroclástico Hundimiento de pumitas |
| Summary: | Pumice clasts present in some detritic sedimentary sequences suggest that they have a density exceeding that of water during transport and accumulation. Because these clasts usually have a density that does not exceed 1g/cm3 and float on water, their behaviour suggests a sinking process to enable them to form part of the sedimentary record.We propose that the most probable mechanism for this is the interaction of pumice clasts at high temperatures with a mass of boiling water. The steam generated would replace the gases in the pores of the pumice by water molecules through micro connections. Subsequent cooling would determine the condensation of the water and the decrease in pressure in the pores. This partial vacuum would result in water absorption, increase in density and in the sinking of the pumice |
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