Class information for: |
Basic class information |
Class id | #P | Avg. number of references |
Database coverage of references |
---|---|---|---|
24681 | 304 | 24.7 | 44% |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
Terms with highest relevance score |
rank | Term | termType | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|---|
1 | DISC LIKE CRYSTAL GROWTH | authKW | 200890 | 1% | 100% | 2 |
2 | FLAT CRYSTAL FACES | authKW | 200890 | 1% | 100% | 2 |
3 | GROWTH FROM HIGH PRESSURE MELT | authKW | 200890 | 1% | 100% | 2 |
4 | ICE CRYSTAL SURFACES | authKW | 200890 | 1% | 100% | 2 |
5 | KINETIC ATTACHMENT | authKW | 200890 | 1% | 100% | 2 |
6 | SURFACE ENERGY REASONS | authKW | 200890 | 1% | 100% | 2 |
7 | NORMAN BRIDGE PHYS | address | 170229 | 3% | 17% | 10 |
8 | 3D REPRODUCTION | authKW | 100445 | 0% | 100% | 1 |
9 | AIR FREE WATER | authKW | 100445 | 0% | 100% | 1 |
10 | ANISOTROPIC KINETIC UNDERCOOLING | authKW | 100445 | 0% | 100% | 1 |
Web of Science journal categories |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | Crystallography | 6187 | 38% | 0% | 117 |
2 | Physics, Applied | 890 | 36% | 0% | 109 |
3 | Materials Science, Multidisciplinary | 759 | 36% | 0% | 110 |
4 | Meteorology & Atmospheric Sciences | 356 | 10% | 0% | 31 |
5 | Physics, Multidisciplinary | 165 | 12% | 0% | 37 |
6 | Chemistry, Physical | 66 | 13% | 0% | 39 |
7 | Physics, Mathematical | 60 | 5% | 0% | 14 |
8 | Physics, Condensed Matter | 24 | 7% | 0% | 21 |
9 | Physics, Fluids & Plasmas | 22 | 3% | 0% | 8 |
10 | Geography, Physical | 12 | 1% | 0% | 4 |
Address terms |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | NORMAN BRIDGE PHYS | 170229 | 3% | 17% | 10 |
2 | QUIM FIS MAT MED AMBIENTE ENERGIA INQUIMAE | 100445 | 0% | 100% | 1 |
3 | LEPMI ELE OCHIM PHYSICOCHIM MAT INTERFA | 50221 | 0% | 50% | 1 |
4 | CREAT TECHNOL ENGN | 50219 | 1% | 25% | 2 |
5 | WATER SUR E STUDIES | 30903 | 1% | 15% | 2 |
6 | LOW TEMP SCI | 18718 | 7% | 1% | 20 |
7 | EDUC EARTH SCI | 16739 | 0% | 17% | 1 |
8 | NASDA | 16737 | 1% | 8% | 2 |
9 | ANTIICING MAT INT | 12554 | 0% | 13% | 1 |
10 | OFF SPACE UTILIZAT SYST | 8369 | 0% | 8% | 1 |
Journals |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
---|---|---|---|---|---|
1 | JOURNAL OF CRYSTAL GROWTH | 18748 | 25% | 0% | 76 |
2 | CRYSTAL RESEARCH AND TECHNOLOGY | 5563 | 6% | 0% | 19 |
3 | JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN | 3892 | 3% | 0% | 10 |
4 | ATMOSPHERIC RESEARCH | 1825 | 3% | 0% | 8 |
5 | ANNALS OF GLACIOLOGY | 973 | 1% | 0% | 4 |
6 | CRYSTAL GROWTH & DESIGN | 937 | 3% | 0% | 9 |
7 | IZVESTIYA SIBIRSKOGO OTDELENIYA AKADEMII NAUK SSSR SERIYA KHIMICHESKIKH NAUK | 828 | 1% | 0% | 3 |
8 | KRISTALL UND TECHNIK-CRYSTAL RESEARCH AND TECHNOLOGY | 516 | 0% | 1% | 1 |
9 | ACTA PHYSICA HUNGARICA | 390 | 0% | 0% | 1 |
10 | JOURNAL DE PHYSIQUE | 371 | 2% | 0% | 6 |
Author Key Words |
Rank | Term | Chi square | Shr. of publ. in class containing term |
Class's shr. of term's tot. occurrences |
#P with term in class |
LCSH search | Wikipedia search |
---|---|---|---|---|---|---|---|
1 | DISC LIKE CRYSTAL GROWTH | 200890 | 1% | 100% | 2 | Search DISC+LIKE+CRYSTAL+GROWTH | Search DISC+LIKE+CRYSTAL+GROWTH |
2 | FLAT CRYSTAL FACES | 200890 | 1% | 100% | 2 | Search FLAT+CRYSTAL+FACES | Search FLAT+CRYSTAL+FACES |
3 | GROWTH FROM HIGH PRESSURE MELT | 200890 | 1% | 100% | 2 | Search GROWTH+FROM+HIGH+PRESSURE+MELT | Search GROWTH+FROM+HIGH+PRESSURE+MELT |
4 | ICE CRYSTAL SURFACES | 200890 | 1% | 100% | 2 | Search ICE+CRYSTAL+SURFACES | Search ICE+CRYSTAL+SURFACES |
5 | KINETIC ATTACHMENT | 200890 | 1% | 100% | 2 | Search KINETIC+ATTACHMENT | Search KINETIC+ATTACHMENT |
6 | SURFACE ENERGY REASONS | 200890 | 1% | 100% | 2 | Search SURFACE+ENERGY+REASONS | Search SURFACE+ENERGY+REASONS |
7 | 3D REPRODUCTION | 100445 | 0% | 100% | 1 | Search 3D+REPRODUCTION | Search 3D+REPRODUCTION |
8 | AIR FREE WATER | 100445 | 0% | 100% | 1 | Search AIR+FREE+WATER | Search AIR+FREE+WATER |
9 | ANISOTROPIC KINETIC UNDERCOOLING | 100445 | 0% | 100% | 1 | Search ANISOTROPIC+KINETIC+UNDERCOOLING | Search ANISOTROPIC+KINETIC+UNDERCOOLING |
10 | BINARY IDEAL SOLUTION | 100445 | 0% | 100% | 1 | Search BINARY+IDEAL+SOLUTION | Search BINARY+IDEAL+SOLUTION |
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. |
Rank | Reference | # ref. in cl. |
Shr. of ref. in cl. |
Citations |
---|---|---|---|---|
1 | LIBBRECHT, KG , (2005) THE PHYSICS OF SNOW CRYSTALS.REPORTS ON PROGRESS IN PHYSICS. VOL. 68. ISSUE 4. P. 855-895 | 32 | 45% | 192 |
2 | ASAKAWA, H , SAZAKI, G , NAGASHIMA, K , NAKATSUBO, S , FURUKAWA, Y , (2016) TWO TYPES OF QUASI-LIQUID LAYERS ON ICE CRYSTALS ARE FORMED KINETICALLY.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA. VOL. 113. ISSUE 7. P. 1749 -1753 | 17 | 59% | 4 |
3 | NELSON, J , (2001) GROWTH MECHANISMS TO EXPLAIN THE PRIMARY AND SECONDARY HABITS OF SNOW CRYSTALS.PHILOSOPHICAL MAGAZINE A-PHYSICS OF CONDENSED MATTER STRUCTURE DEFECTS AND MECHANICAL PROPERTIES. VOL. 81. ISSUE 10. P. 2337-2373 | 27 | 68% | 25 |
4 | RICKERBY, ME , LIBBRECHT, KG , (2013) MEASUREMENTS OF SURFACE ATTACHMENT KINETICS FOR FACETED ICE CRYSTAL GROWTH.JOURNAL OF CRYSTAL GROWTH. VOL. 377. ISSUE . P. 1 -8 | 16 | 73% | 5 |
5 | ASAKAWA, H , SAZAKI, G , NAGASHIMA, K , NAKATSUBO, S , FURUKAWA, Y , (2015) PRISM AND OTHER HIGH-INDEX FACES OF ICE CRYSTALS EXHIBIT TWO TYPES OF QUASI-LIQUID LAYERS.CRYSTAL GROWTH & DESIGN. VOL. 15. ISSUE 7. P. 3339 -3344 | 16 | 62% | 3 |
6 | NANEV, CN , (1997) POLYHEDRAL INSTABILITY - SKELETAL AND DENDRITIC GROWTH.PROGRESS IN CRYSTAL GROWTH AND CHARACTERIZATION OF MATERIALS. VOL. 35. ISSUE 1. P. 1 -26 | 23 | 70% | 22 |
7 | SHIMADA, W , OHTAKE, K , (2016) THREE-DIMENSIONAL MORPHOLOGY OF NATURAL SNOW CRYSTALS.CRYSTAL GROWTH & DESIGN. VOL. 16. ISSUE 10. P. 5603 -5605 | 9 | 100% | 0 |
8 | ASAKAWA, H , SAZAKI, G , YOKOYAMA, E , NAGASHIMA, K , NAKATSUBO, S , FURUKAWA, Y , (2014) ROLES OF SURFACE/VOLUME DIFFUSION IN THE GROWTH KINETICS OF ELEMENTARY SPIRAL STEPS ON ICE BASAL FACES GROWN FROM WATER VAPOR.CRYSTAL GROWTH & DESIGN. VOL. 14. ISSUE 7. P. 3210 -3220 | 17 | 53% | 2 |
9 | GRAVNER, J , GRIFFEATH, D , (2009) MODELING SNOW-CRYSTAL GROWTH: A THREE-DIMENSIONAL MESOSCOPIC APPROACH.PHYSICAL REVIEW E. VOL. 79. ISSUE 1. P. - | 14 | 61% | 17 |
10 | LIBBRECHT, KG , (2003) EXPLAINING THE FORMATION OF THIN ICE CRYSTAL PLATES WITH STRUCTURE-DEPENDENT ATTACHMENT KINETICS.JOURNAL OF CRYSTAL GROWTH. VOL. 258. ISSUE 1-2. P. 168-175 | 13 | 76% | 20 |
Classes with closest relation at Level 1 |