2009 Fourth ChinaGrid Annual Conference 2009
DOI: 10.1109/chinagrid.2009.9
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MPICH-G-DM: An Enhanced MPICH-G with Supporting Dynamic Job Migration

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Cited by 4 publications
(3 citation statements)
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“…The particle size homogeneity and smoothness were improved and mean particle diameters decreased by increasing the surfactant (PVA) concentration as also observed by other researchers. 14,35,36 Smaller microspheres have been previously reported with the use of surfactant during the preparation of microspheres due to the amphiphilic behavior of the surfactant (PVA). [37][38][39][40] Further optimization involved use of gelatin in the preparation of microspheres, from 1 to 3% (w/v) and at different temperatures (37 and 45 C) for preventing gellation.…”
Section: Resultsmentioning
confidence: 99%
“…The particle size homogeneity and smoothness were improved and mean particle diameters decreased by increasing the surfactant (PVA) concentration as also observed by other researchers. 14,35,36 Smaller microspheres have been previously reported with the use of surfactant during the preparation of microspheres due to the amphiphilic behavior of the surfactant (PVA). [37][38][39][40] Further optimization involved use of gelatin in the preparation of microspheres, from 1 to 3% (w/v) and at different temperatures (37 and 45 C) for preventing gellation.…”
Section: Resultsmentioning
confidence: 99%
“…The CE-1 data have channel-dependent resolutions of ~35 -50 km from its orbital altitude of ~200 km, while the CE-2 data have resolutions of ~17.5 -25 km because its orbital altitude was ~100 km. The microwave observations have been used to estimate regolith thickness [39] , dielectric properties [15,16,40] , rock abundance [41,42] , subsurface temperatures [43] , and geothermal heat flow [44,45] as well as the eruption phase of basaltic volcanism in the Mare of the Moon [46] . In the polar region, MRM data analysis usually focuses on searching for evidence of water ice [47] and studying the thermal gradient [48] .…”
Section: Methods: 1: Instrument Background and Loss Tangent Mapsmentioning
confidence: 99%
“…The CE-1 data have channel-dependent resolutions of ~35 -50 km from its orbital altitude of ~200 km, while the CE-2 data have resolutions of ~17.5 -25 km because its orbital altitude was ~100 km. The microwave observations have been used to estimate regolith thickness [39] , dielectric properties [15,16,40] , rock abundance [41,42] , subsurface temperatures [43] , and geothermal heat flow [44,45] as well as the eruption phase of basaltic volcanism in the Mare of the Moon [46] . In the polar region, MRM data analysis usually focuses on searching for evidence of water ice [47] and studying the thermal gradient [48] .…”
Section: Methods: 1: Instrument Background and Loss Tangent Mapsmentioning
confidence: 99%