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Critical roles of short-range-order minerals in shaping soil water retention curves in volcanic regions

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F25%3A00640577" target="_blank" >RIV/60077344:_____/25:00640577 - isvavai.cz</a>

  • Result on the web

    <a href="https://acsess.onlinelibrary.wiley.com/doi/pdfdirect/10.1002/vzj2.70036" target="_blank" >https://acsess.onlinelibrary.wiley.com/doi/pdfdirect/10.1002/vzj2.70036</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/vzj2.70036" target="_blank" >10.1002/vzj2.70036</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Critical roles of short-range-order minerals in shaping soil water retention curves in volcanic regions

  • Original language description

    Predicting water retention is difficult for highly aggregated volcanic soils (Andisols) with heterogeneous pore size distribution. This paper aimed to examine how andic materials influence soil water retention based on soil composition. We compiled the data of water retention in the soils from literature with physicochemical properties and soil constituents (organic matter, sand, silt, crystalline clay, and short-range-order mineral fractions) to obtain the parameters of water retention curve models (van Genuchten, Durner, and Assouline). The pedo-transfer functions were successfully constructed in the van Genuchten and Assouline models with bulk density, pH, soil C, cation exchange capacity, sand content, and andic property, but the direct estimation from soil composition (clay content, sand content, soil C, oxalate extractable Al, Fe, and Si) achieved the better prediction of soil water retention curves. Organic matter increases plant-available water retention (pF 1.5–4.2), while short-range-order minerals in volcanic soils enhance water retention at pF 4.2–7.0. This is caused by the larger volume of finer micropore (av. 0.012 µm in diameter) in volcanic soils, compared to non-volcanic soils (av. 0.020 µm). Our study highlights the importance of including andic properties (oxalate-extractable aluminum and iron) to improve prediction of soil water retention in volcanic regions, although soil water retention could roughly be predicted by sand content at the global scale.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    40104 - Soil science

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Vadose Zone Journal

  • ISSN

    1539-1663

  • e-ISSN

    1539-1663

  • Volume of the periodical

    24

  • Issue of the periodical within the volume

    5

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    17

  • Pages from-to

    e70036

  • UT code for WoS article

    001605588200005

  • EID of the result in the Scopus database

    2-s2.0-105016452770