VADOSE ZONE JOURNAL

metrics 2024

Exploring innovative methodologies in soil research.

Introduction

Vadose Zone Journal, published by Wiley, is a premier Open Access journal dedicated to advancing research in the dynamic field of soil science, particularly focusing on the vadose zone—the area of soil above the groundwater table that plays a critical role in hydrological processes. Since its inception in 2002, the journal has provided a platform for high-quality, impactful research, reflected in its impressive ranking among the top 25% of journals in the Soil Science category. With an increasing emphasis on sustainable agricultural practices and environmental protection, the Vadose Zone Journal offers invaluable insights and innovative methodologies that cater to the needs of researchers, practitioners, and students alike. Located in Hoboken, NJ, the journal operates on a fully Open Access model since 2018, ensuring that cutting-edge findings are readily accessible to a global audience. Join the community of experts and make significant contributions to our understanding of critical soil processes through this esteemed publication.

Metrics 2024

SCIMAGO Journal Rank-
Journal Impact Factor2.50
Journal Impact Factor (5 years)3.30
H-Index-
Journal IF Without Self2.50
Eigen Factor0.00
Normal Eigen Factor0.70
Influence0.84
Immediacy Index0.40
Cited Half Life10.40
Citing Half Life11.30
JCI0.60
Total Documents-
WOS Total Citations5312
SCIMAGO Total Citations-
SCIMAGO SELF Citations-
Scopus Journal Rank-
Cites / Document (2 Years)-
Cites / Document (3 Years)-
Cites / Document (4 Years)-

Metrics History

Rank 2024

IF (Web Of Science)

ENVIRONMENTAL SCIENCES
Rank 209/358
Percentile 41.80
Quartile Q3
SOIL SCIENCE
Rank 23/49
Percentile 54.10
Quartile Q2
WATER RESOURCES
Rank 54/127
Percentile 57.90
Quartile Q2

JCI (Web Of Science)

ENVIRONMENTAL SCIENCES
Rank 188/359
Percentile 47.63
Quartile Q3
SOIL SCIENCE
Rank 25/49
Percentile 48.98
Quartile Q3
WATER RESOURCES
Rank 57/127
Percentile 55.12
Quartile Q2

Quartile History

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