更正“农业土壤中的石球：与岩石碎片连接岩石和土壤有关的微生境”

IF 4 2区农林科学 Q2 SOIL SCIENCE

European Journal of Soil Science Pub Date : 2025-02-28 DOI:10.1111/ejss.70066

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引用次数: 0

摘要

迪特里希，F.， B. Klaes， L.勃兰特，N. Groschopf， S. Thiele-Bruhn。2024. 农业土壤中的石球：一个与岩石碎片连接岩石和土壤相关的微栖息地。土壤科学通报，30(6),344 - 344。https://doi.org/10.1111/ejss.70025.The图2的标题不正确。图2的正确标题是：化学风化与元素迁移、OM积累和非晶铁（氢）氧化物产生之间的关系，指向风化岩石和土壤中微栖息地的演化。(a)由锆浓度和钡铌比表明的重矿物的物理积累和元素因化学风化而耗竭。(b) Feo浓度和δ13C值表明，随着OM含量的增加，非晶铁（氢）氧化物富集。插入CaCO3和om源碳（C3植物）的典型δ13C范围（Hoefs 2009）。δ13C和传质系数τZr的变化描述了随着OM含量和周转率的增加，Fe (c)和Si (d)的部分损失。我们为这个错误道歉。

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Correction to “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil”

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) Fe_o 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 (τ_Zr) depict the fractional loss of Fe (c) and Si (d) with increasing OM content and turnover rates. We apologize for this error.

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来源期刊

European Journal of Soil Science 农林科学-土壤科学

CiteScore

8.20

自引率

4.80%

发文量

117

审稿时长

5 months

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.