Class information for: |
Basic class information |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
| Cluster id | Level | Cluster label | #P |
|---|---|---|---|
| 3 | 4 | GEOSCIENCES, MULTIDISCIPLINARY//GEOCHEMISTRY & GEOPHYSICS//METEOROLOGY & ATMOSPHERIC SCIENCES | 1953906 |
| 123 | 3 | ENGINEERING, GEOLOGICAL//JOURNAL OF GEOTECHNICAL AND GEOENVIRONMENTAL ENGINEERING//ENGINEERING, PETROLEUM | 69565 |
| 2272 | 2 | GEOSYNTHETIC CLAY LINER//BENTONITE//GEOMEMBRANE | 4889 |
| 27264 | 1 | HYBRID MIXTURE THEORY//DISJOINING SWELLING PRESSURE//MODIFIED TERZAGHIS PRINCIPLE | 254 |
Terms with highest relevance score |
| rank | Category | termType | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|---|
| 1 | HYBRID MIXTURE THEORY | authKW | 610858 | 3% | 62% | 8 |
| 2 | DISJOINING SWELLING PRESSURE | authKW | 496327 | 2% | 100% | 4 |
| 3 | MODIFIED TERZAGHIS PRINCIPLE | authKW | 372245 | 1% | 100% | 3 |
| 4 | SWELLING POROUS MEDIA | authKW | 343605 | 2% | 46% | 6 |
| 5 | BIOPOLYMERIC | authKW | 248164 | 1% | 100% | 2 |
| 6 | COUPLING OF FLUID AND SOLID MOTIONS | authKW | 248164 | 1% | 100% | 2 |
| 7 | DOUBLE LAYER REPULSIVE FORCE | authKW | 248164 | 1% | 100% | 2 |
| 8 | MODELISAT MESOSCOP CHIM THEOR LMCT | address | 248164 | 1% | 100% | 2 |
| 9 | SWELLING TISSUE | authKW | 248164 | 1% | 100% | 2 |
| 10 | VANT HOFF LAW | authKW | 248164 | 1% | 100% | 2 |
Web of Science journal categories |
| chi_square_rank | Category | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | Engineering, Geological | 1823 | 10% | 0% | 26 |
| 2 | Engineering, Chemical | 679 | 22% | 0% | 57 |
| 3 | Mechanics | 554 | 17% | 0% | 43 |
| 4 | Engineering, General | 215 | 7% | 0% | 19 |
| 5 | Geosciences, Multidisciplinary | 161 | 10% | 0% | 26 |
| 6 | Water Resources | 84 | 6% | 0% | 14 |
| 7 | Computer Science, Interdisciplinary Applications | 83 | 6% | 0% | 14 |
| 8 | Limnology | 59 | 2% | 0% | 5 |
| 9 | Mathematics, Applied | 47 | 7% | 0% | 17 |
| 10 | Mathematics, Interdisciplinary Applications | 47 | 4% | 0% | 9 |
Address terms |
| chi_square_rank | term | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | MODELISAT MESOSCOP CHIM THEOR LMCT | 248164 | 1% | 100% | 2 |
| 2 | ENSCM MARCOULE | 165441 | 1% | 67% | 2 |
| 3 | CEAICSM UMR 5257 MODELISAT MESOSCOP CHIM T | 124082 | 0% | 100% | 1 |
| 4 | CEAICSMLMCTUMR 5257 | 124082 | 0% | 100% | 1 |
| 5 | CNRS PHENIX UMR 8234 | 124082 | 0% | 100% | 1 |
| 6 | CONMPUTAT MATH | 124082 | 0% | 100% | 1 |
| 7 | EVALUAT SURETE | 124082 | 0% | 100% | 1 |
| 8 | ICSM UMR 5257CNRSENSCM MARCOULE | 124082 | 0% | 100% | 1 |
| 9 | ICSMENSCM MARCOULECEA | 124082 | 0% | 100% | 1 |
| 10 | INPG LTHE | 124082 | 0% | 100% | 1 |
Journals |
| chi_square_rank | term | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | TRANSPORT IN POROUS MEDIA | 78986 | 17% | 1% | 44 |
| 2 | INTERNATIONAL JOURNAL OF ENGINEERING SCIENCE | 5540 | 6% | 0% | 14 |
| 3 | COMPUTERS AND GEOTECHNICS | 3153 | 3% | 0% | 7 |
| 4 | FF COMMUNICATIONS | 2952 | 0% | 2% | 1 |
| 5 | COMPUTATIONAL GEOSCIENCES | 1528 | 1% | 0% | 3 |
| 6 | MECHANICS OF COHESIVE-FRICTIONAL MATERIALS | 1441 | 0% | 1% | 1 |
| 7 | JOURNAL OF COLLOID AND INTERFACE SCIENCE | 1433 | 7% | 0% | 17 |
| 8 | GEOTECHNIQUE | 1371 | 2% | 0% | 5 |
| 9 | INTERNATIONAL JOURNAL FOR NUMERICAL AND ANALYTICAL METHODS IN GEOMECHANICS | 1317 | 2% | 0% | 5 |
| 10 | COMPTES RENDUS MECANIQUE | 1310 | 2% | 0% | 4 |
Author Key Words |
Core articles |
The table includes core articles in the class. The following variables is taken into account for the relevance score of an article in a cluster c: (1) Number of references referring to publications in the class. (2) Share of total number of active references referring to publications in the class. (3) Age of the article. New articles get higher score than old articles. (4) Citation rate, normalized to year. |
Classes with closest relation at Level 1 |