Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling

Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value....
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Autor*in:	Yokoyama, Tadashi [verfasserIn] Nomura, Ryoto Nishiyama, Naoki

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	Capillary rise Pore radius distribution Air entrapment Sandstone

Anmerkung:	© The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Übergeordnetes Werk:	Enthalten in: Transport in porous media - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986, 148(2023), 1 vom: 29. März, Seite 67-93
Übergeordnetes Werk:	volume:148 ; year:2023 ; number:1 ; day:29 ; month:03 ; pages:67-93

Links:	Volltext

DOI / URN:	10.1007/s11242-023-01915-7

Katalog-ID:	SPR050325264

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520			\|a Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown.
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allfields	10.1007/s11242-023-01915-7 doi (DE-627)SPR050325264 (SPR)s11242-023-01915-7-e DE-627 ger DE-627 rakwb eng Yokoyama, Tadashi verfasserin (orcid)0000-0003-3294-3882 aut Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models Capillary rise (dpeaa)DE-He213 Pore radius distribution (dpeaa)DE-He213 Air entrapment (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Nomura, Ryoto aut Nishiyama, Naoki aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 148(2023), 1 vom: 29. März, Seite 67-93 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:148 year:2023 number:1 day:29 month:03 pages:67-93 https://dx.doi.org/10.1007/s11242-023-01915-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 148 2023 1 29 03 67-93
spelling	10.1007/s11242-023-01915-7 doi (DE-627)SPR050325264 (SPR)s11242-023-01915-7-e DE-627 ger DE-627 rakwb eng Yokoyama, Tadashi verfasserin (orcid)0000-0003-3294-3882 aut Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models Capillary rise (dpeaa)DE-He213 Pore radius distribution (dpeaa)DE-He213 Air entrapment (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Nomura, Ryoto aut Nishiyama, Naoki aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 148(2023), 1 vom: 29. März, Seite 67-93 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:148 year:2023 number:1 day:29 month:03 pages:67-93 https://dx.doi.org/10.1007/s11242-023-01915-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 148 2023 1 29 03 67-93
allfields_unstemmed	10.1007/s11242-023-01915-7 doi (DE-627)SPR050325264 (SPR)s11242-023-01915-7-e DE-627 ger DE-627 rakwb eng Yokoyama, Tadashi verfasserin (orcid)0000-0003-3294-3882 aut Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models Capillary rise (dpeaa)DE-He213 Pore radius distribution (dpeaa)DE-He213 Air entrapment (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Nomura, Ryoto aut Nishiyama, Naoki aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 148(2023), 1 vom: 29. März, Seite 67-93 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:148 year:2023 number:1 day:29 month:03 pages:67-93 https://dx.doi.org/10.1007/s11242-023-01915-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 148 2023 1 29 03 67-93
allfieldsGer	10.1007/s11242-023-01915-7 doi (DE-627)SPR050325264 (SPR)s11242-023-01915-7-e DE-627 ger DE-627 rakwb eng Yokoyama, Tadashi verfasserin (orcid)0000-0003-3294-3882 aut Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models Capillary rise (dpeaa)DE-He213 Pore radius distribution (dpeaa)DE-He213 Air entrapment (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Nomura, Ryoto aut Nishiyama, Naoki aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 148(2023), 1 vom: 29. März, Seite 67-93 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:148 year:2023 number:1 day:29 month:03 pages:67-93 https://dx.doi.org/10.1007/s11242-023-01915-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 148 2023 1 29 03 67-93
allfieldsSound	10.1007/s11242-023-01915-7 doi (DE-627)SPR050325264 (SPR)s11242-023-01915-7-e DE-627 ger DE-627 rakwb eng Yokoyama, Tadashi verfasserin (orcid)0000-0003-3294-3882 aut Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models Capillary rise (dpeaa)DE-He213 Pore radius distribution (dpeaa)DE-He213 Air entrapment (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213 Nomura, Ryoto aut Nishiyama, Naoki aut Enthalten in Transport in porous media Dordrecht [u.a.] : Springer Science + Business Media B.V, 1986 148(2023), 1 vom: 29. März, Seite 67-93 (DE-627)269017720 (DE-600)1473676-7 1573-1634 nnns volume:148 year:2023 number:1 day:29 month:03 pages:67-93 https://dx.doi.org/10.1007/s11242-023-01915-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 148 2023 1 29 03 67-93
language	English
source	Enthalten in Transport in porous media 148(2023), 1 vom: 29. März, Seite 67-93 volume:148 year:2023 number:1 day:29 month:03 pages:67-93
sourceStr	Enthalten in Transport in porous media 148(2023), 1 vom: 29. März, Seite 67-93 volume:148 year:2023 number:1 day:29 month:03 pages:67-93
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Capillary rise Pore radius distribution Air entrapment Sandstone
isfreeaccess_bool	false
container_title	Transport in porous media
authorswithroles_txt_mv	Yokoyama, Tadashi @@aut@@ Nomura, Ryoto @@aut@@ Nishiyama, Naoki @@aut@@
publishDateDaySort_date	2023-03-29T00:00:00Z
hierarchy_top_id	269017720
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author	Yokoyama, Tadashi
spellingShingle	Yokoyama, Tadashi misc Capillary rise misc Pore radius distribution misc Air entrapment misc Sandstone Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling
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topic_title	Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling Capillary rise (dpeaa)DE-He213 Pore radius distribution (dpeaa)DE-He213 Air entrapment (dpeaa)DE-He213 Sandstone (dpeaa)DE-He213
topic	misc Capillary rise misc Pore radius distribution misc Air entrapment misc Sandstone
topic_unstemmed	misc Capillary rise misc Pore radius distribution misc Air entrapment misc Sandstone
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format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
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title	Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling
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title_full	Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling
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author_browse	Yokoyama, Tadashi Nomura, Ryoto Nishiyama, Naoki
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title_sort	size distributions of water and air in rock pores induced by capillary rise: experiments and modeling
title_auth	Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling
abstract	Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
abstractGer	Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
abstract_unstemmed	Abstract For predicting the size distributions of water and air induced by capillary rise of water in rock, two previous concepts are applicable. One model uses the assumption that pores are filled with water in the order of smallest to largest pores until the water saturation reaches a given value. Another model is based on Parker and Lenhard (Water Resour Res 23:2187–2196, 1987) where for any pore radius air is trapped at the same water/air ratio. In both models, water saturation after capillary rise as well as pore radius distribution need to be known. We developed a model that can predict the size distributions of water and air by using pore radius distribution alone. Our model considers which way water will go when the flow path branches into a large path and a small path. The size distributions of water and air predicted by our model and the other models were compared with those experimentally determined by the water expulsion method. Our model tended to overestimate the amount of water in smaller pores and underestimate that in larger pores if only the effect of branching of pore was considered. The reproducibility of experimental results became comparable to or better than other models by adding to our model the effect that the amount of water entering the small path is reduced for compensating for the effect of bulging of path. Our model is useful in predicting how water enters in pores even when water saturation is unknown. Article Highlights Which pores are filled with water and air during capillary rise was investigated by experiments and model calculationsOur model evaluates for all pore radii combinations which way the water will go at the branching point of poresEven if water saturation as required by other models is unknown, our model's predictions were comparable to other models © The Author(s), under exclusive licence to Springer Nature B.V. 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
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title_short	Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling
url	https://dx.doi.org/10.1007/s11242-023-01915-7
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author2	Nomura, Ryoto Nishiyama, Naoki
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doi_str	10.1007/s11242-023-01915-7
up_date	2024-07-03T14:49:34.723Z
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Size Distributions of Water and Air in Rock Pores Induced by Capillary Rise: Experiments and Modeling

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