2000
DOI: 10.1016/s0920-4105(00)00010-3
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Spontaneous imbibition characteristics of diatomite

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Cited by 213 publications
(160 citation statements)
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“…It was observed that the water imbibed into the smaller pores and the air was ejected from the larger pores. The production flow paths of air were smaller in dimension, which is agreement with experimental results of high water saturation behind the imbibition front by use of diatomite samples (Akin et al, 2000). Babadagli (2008, 2010) conducted the similar visualization experiments by use of two-dimensional sandpacks and micromodels to clarify the physics of SI at pore scale.…”
Section: Micromodels For Spontaneous Imbibitionsupporting
confidence: 76%
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“…It was observed that the water imbibed into the smaller pores and the air was ejected from the larger pores. The production flow paths of air were smaller in dimension, which is agreement with experimental results of high water saturation behind the imbibition front by use of diatomite samples (Akin et al, 2000). Babadagli (2008, 2010) conducted the similar visualization experiments by use of two-dimensional sandpacks and micromodels to clarify the physics of SI at pore scale.…”
Section: Micromodels For Spontaneous Imbibitionsupporting
confidence: 76%
“…Therefore, the snap-off of air was suppressed by the rapid SI of water. Akin et al (2000) reported the similar experimental results using X-ray imaging to study the SI in diatomite samples. In instantly filled fracture experiments, little water was drawn into the matrix system before the fracture was filled with water and non-wetting phase was ejected from the matrix system counter-currently.…”
Section: Micromodels For Spontaneous Imbibitionsupporting
confidence: 56%
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