Text Correction
The authors wish to make the following corrections to their paper [1]. We wish to make the following correction:
Section 2.4 (Determination of Ks), Paragraph 1, due to errors in the detailed description methods added in the revised version, “The soil samples were soaked in water for 12 h to reach saturation, and placed on coarse sand for 12 h to reach field water capacity. The height of the water head was controlled to be 2 cm by the Markov bottle (Figure 3).” The measurement process of Ks should actually be “The soil samples were soaked in water for 12 h to reach saturation. The height of the water head was controlled to be 2 cm by the Markov bottle (Figure 3).” We noticed this error after the manuscript was received, and to avoid misleading readers, we have corrected this part of the description. However, this description has no effect on the results of the article, as our actual operation procedure is correct.
The authors would like to apologize for any inconvenience caused to the readers by the change. The authors state that the scientific conclusions are unaffected. This correction was approved by the Academic Editor. The original publication has also been updated.
Reference
- Wang, D.; Niu, J.; Miao, Y.; Yang, T.; Berndtsson, R. Predicting Soil Saturated Water Conductivity Using Pedo-Transfer Functions for Rocky Mountain Forests in Northern China. Forests 2023, 14, 1097. [Google Scholar] [CrossRef]
Disclaimer/Publisher’s Note: The statements, opinions and data contained in all publications are solely those of the individual author(s) and contributor(s) and not of MDPI and/or the editor(s). MDPI and/or the editor(s) disclaim responsibility for any injury to people or property resulting from any ideas, methods, instructions or products referred to in the content. |
© 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).