Critical Supersaturation
Critical Supersaturation is a theoretical threshold in scale control mechanisms, defined as the minimum level of supersaturation required to initiate spontaneous nucleation of scale-forming minerals, distinguishing it from subcritical conditions that inhibit precipitate formation.
416
Publications
23.4K
Citations
1.1K
Authors
432
Institutions
Publications per year
2017–2026
51
Parents
416
Review: Nucleation in solutions revisited
Dimo Kashchiev, G.M. van Rosmalen · Crystal Research and Technology · 2003 · 665 citations
Natural Sciences, Chemistry, Physics +15
Reconsiderations of Nucleation Theory
J. Lothe, G. M. Pound · The Journal of Chemical Physics · 1962 · 575 citations
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432

University of Rochester
Rochester, United States
9 h-index
23 publications
999 citations
Georgia Institute of Technology
Atlanta, United States
8 h-index
20 publications
1.6K citations
Colorado State University
Fort Collins, United States
7 h-index
12 publications
781 citations

NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
6 publications
469 citations
Desert Research Institute
Reno, United States
6 h-index
9 publications
520 citations

Tohoku University
Sendai, Japan
6 h-index
10 publications
330 citations
University of Copenhagen
Copenhagen, Denmark
6 h-index
19 publications
1.1K citations

Bulgarian Academy of Sciences
Sofia, Bulgaria
5 h-index
7 publications
334 citations
1–8 of 432
58 publications · 5.3K citations
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23 publications · 869 citations
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19 publications · 641 citations
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JGR · 13 publications · 1.5K citations
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10 publications · 1.1K citations
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