{"title":"Correction to “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil”","authors":"","doi":"10.1111/ejss.70066","DOIUrl":null,"url":null,"abstract":"<p>Dittrich, F., B. Klaes, L. Brandt, N. Groschopf, S. Thiele-Bruhn. 2024. “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil.” <i>European Journal of Soil Science</i> 75(6), e70025. https://doi.org/10.1111/ejss.70025.</p><p>The caption for Figure 2 is incorrect. The correct caption for Figure 2 is: Relationships between chemical weathering and element mobility, OM accumulation and the production of noncrystalline Fe-(hydr)oxides pointing towards the evolution of a microhabitat in weathered rocks and soils. (a) Physical accumulation of heavy minerals and element depletion through chemical weathering as indicated by Zr concentrations and Ba:Nb ratios. (b) Fe<sub>o</sub> concentrations and δ<sup>13</sup>C values indicate an enrichment in noncrystalline Fe-(hydr)oxides with increasing OM content. Typical δ<sup>13</sup>C ranges for CaCO<sub>3</sub> and OM-sourced carbon (C3 plants) are inserted (Hoefs 2009). Variations in δ<sup>13</sup>C and mass transfer coefficients (<i>τ</i><sub>Zr</sub>) depict the fractional loss of Fe (c) and Si (d) with increasing OM content and turnover rates. We apologize for this error.</p>","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"76 2","pages":""},"PeriodicalIF":4.0000,"publicationDate":"2025-02-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1111/ejss.70066","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"European Journal of Soil Science","FirstCategoryId":"97","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/ejss.70066","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0
Abstract
Dittrich, F., B. Klaes, L. Brandt, N. Groschopf, S. Thiele-Bruhn. 2024. “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil.” European Journal of Soil Science 75(6), e70025. https://doi.org/10.1111/ejss.70025.
The caption for Figure 2 is incorrect. The correct caption for Figure 2 is: Relationships between chemical weathering and element mobility, OM accumulation and the production of noncrystalline Fe-(hydr)oxides pointing towards the evolution of a microhabitat in weathered rocks and soils. (a) Physical accumulation of heavy minerals and element depletion through chemical weathering as indicated by Zr concentrations and Ba:Nb ratios. (b) Feo concentrations and δ13C values indicate an enrichment in noncrystalline Fe-(hydr)oxides with increasing OM content. Typical δ13C ranges for CaCO3 and OM-sourced carbon (C3 plants) are inserted (Hoefs 2009). Variations in δ13C and mass transfer coefficients (τZr) depict the fractional loss of Fe (c) and Si (d) with increasing OM content and turnover rates. We apologize for this error.
期刊介绍:
The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.