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Corrigendum: Effects of freeze-thaw cycles on the size distribution and stability of soil aggregate in the permafrost regions of the Qinghai-Tibetan Plateau (2023 Environ. Res. Commun.5 095008)

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Published 7 December 2023 © 2023 The Author(s). Published by IOP Publishing Ltd
, , Citation Chenjie Dong et al 2023 Environ. Res. Commun. 5 129501 DOI 10.1088/2515-7620/acfd8b

This is a correction for 2023 Environ. Res. Commun. 5 095008

2515-7620/5/12/129501

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Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.

Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.

The typographical for table 2 in [Dong et al 2023 Environ. Res. Commun. 5 095008] contain some mistakes which are corrected in this corrigendum.

PeriodsSoil layerThawing periodCompletely thawed periodFreezing periodCompletely frozen period
Sand (%)0–10 cm43.91 ± 1.29a50.05 ± 5.06a49.64 ± 5.64a43.54 ± 3.64a
 10–20 cm38.59 ± 2.9a40.75 ± 2.81a41.65 ± 1.46a39.88 ± 1.01a
Silt (%)0–10 cm43.71 ± 0.17a38.59 ± 2.97a39.77 ± 3.76a43.21 ± 1.32a
 10–20 cm47.56 ± 2.55a44.05 ± 1.9a45.3 ± 1.88a43.16 ± 1.98a
Clay (%)0–10 cm12.39 ± 1.16a11.36 ± 2.22a10.59 ± 1.88a13.25 ± 2.37a
 10–20 cm13.85 ± 0.37ab15.21 ± 1.19ab13.05 ± 0.57b16.95 ± 1.61a
pH0–10 cm8.79 ± 0.07a8.84 ± 0.05a8.91 ± 0.15a8.77 ± 0.16a
 10–20 cm8.96 ± 0.08a8.78 ± 0.13a8.8 ± 0.08a8.78 ± 0.08a
Eh (μV)0–10 cm188.67 ± 21.62a178 ± 5.51a211.67 ± 6.69a173.67 ± 27.14a
 10–20 cm201.67 ± 10.27a206 ± 1.73a183.67 ± 5.36a179.67 ± 23.9a
MBC (mg·kg−1)0–10 cm186.68 ± 26.53a363.11 ± 5.69a255.58 ± 116.15a196.52 ± 21.04a
 10–20 cm170.16 ± 25.88a240.01 ± 118.96a124.28 ± 23.57a83.48 ± 6.63a
MBN (mg·kg−1)0–10 cm14.99 ± 3.32a11.6 ± 3.13a15.58 ± 3.2a16.94 ± 4.8a
 10–20 cm9.21 ± 0.43a7.03 ± 2.37ab4.05 ± 0.86b7.83 ± 0.48ab
SOM (g·kg−1)0–10 cm30.32 ± 7.85a40.67 ± 14.2a40.05 ± 11.34a28.8 ± 6.99a
 10–20 cm23.09 ± 3.11a22.55 ± 3.13a19.14 ± 1.92a21.39 ± 2.76a
IC (g·kg−1)0–10 cm15.56 ± 1.81a16.89 ± 1.52a14.67 ± 0.8a16.18 ± 0.7a
 10–20 cm18.79 ± 3.66a18.03 ± 1.27a18.82 ± 1.18a18.92 ± 2.01a
NH4 +-N (mg·N·L−1)0–10 cm8.72 ± 4.66ab17.19 ± 1.41a11.69 ± 2.36ab4.64 ± 1.73b
 10–20 cm3.4 ± 0.32a16.49 ± 0.07a15.71 ± 1.23a3.47 ± 0.14a
NO3 --N (mg·N·L−1)0–10 cm5.41 ± 0.78a4.36 ± 1.57a4.54 ± 2.76a2.86 ± 0.82a
 10–20 cm1.19 ± 0.59a1.18 ± 0.65a2.27 ± 1.19a2.17 ± 1.13a
BGB (kg·m−2)0–10 cm3.57 ± 0.43a5.22 ± 1.02a2.70 ± 1.00a5.93 ± 2.06a
 10–20 cm0.29 ± 0.08a0.1 ± 0.01a0.59 ± 0.21a1.04 ± 0.56a

The numerical results and conclusions in table 2 remain unchanged.

Acknowledgments

This work was supported by 'Light of the West' Cross-team Project of the Chinese Academy of Sciences (xbzgzdsys-202214), the National Natural Science Foundation of China (41871064), Gansu Provincial Science and Technology Program (22ZD6FA005) and Qinghai Province High-level Innovative 'Thousand Talents' Program.

Data availability statement

The data cannot be made publicly available upon publication because no suitable repository exists for hosting data in this field of study. The data that support the findings of this study are available upon reasonable request from the authors.

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