黄土高原自然植被恢复过程中土壤温度和水分的相关性

王俊; 郭金龙; 张永旺; 魏瑶瑶; 郑恩

doi:10.13870/j.cnki.stbcxb.2022.02.017

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黄土高原自然植被恢复过程中土壤温度和水分的相关性

更新时间：2024-11-07

- 黄土高原自然植被恢复过程中土壤温度和水分的相关性
- The Correlation Between Soil Temperature and Water Content During the Natural Vegetation Restoration on the Loess Plateau
- 水土保持学报 2022年36卷第2期页码：130-137
- 作者机构：
  
  1. 延安大学生命科学学院,陕西,延安,716000
  2. 西北农林科技大学植物保护学院, 农业部西北黄土高原作物有害生物综合治理重点实验室, 陕西杨凌,712100
  3. 陕西省红枣重点实验室(延安大学),陕西,延安,716000
- 作者简介：
  
  [ "王俊(1987-),女,硕士研究生,主要从事土壤生态研究。E-mail:wangjun6082@163.com" ]
- 基金信息：
  
  国家自然科学基金项目（41807520）延安大学科研项目（YDQ2018-21）博士科研启动项目（YDBK2017-25）创新能力支撑计划项目（2020KJXX-009）
- DOI：10.13870/j.cnki.stbcxb.2022.02.017
  中图分类号： S152
- 纸质出版：2022
- 稿件说明：
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王俊, 郭金龙, 张永旺, 等. 黄土高原自然植被恢复过程中土壤温度和水分的相关性[J]. 水土保持学报, 2022,36(2):130-137.

WANG Jun, GUO Jinlong, ZHANG Yongwang, et al. The Correlation Between Soil Temperature and Water Content During the Natural Vegetation Restoration on the Loess Plateau[J]. 2022, 36(2): 130-137.
王俊, 郭金龙, 张永旺, 等. 黄土高原自然植被恢复过程中土壤温度和水分的相关性[J]. 水土保持学报, 2022,36(2):130-137. DOI： 10.13870/j.cnki.stbcxb.2022.02.017.

WANG Jun, GUO Jinlong, ZHANG Yongwang, et al. The Correlation Between Soil Temperature and Water Content During the Natural Vegetation Restoration on the Loess Plateau[J]. 2022, 36(2): 130-137. DOI： 10.13870/j.cnki.stbcxb.2022.02.017.

摘要

土壤水热因子是影响作物生长发育的重要因子

尤其是在黄土高原自然植被恢复过程中。通过对黄土高原不同自然植被恢复阶段的土壤水分和温度的长期监测

研究植被恢复过程中土壤温度和水分的动态变化及其相关性。结果表明:8-10月草地群落的土壤温度显著高于其他群落

11月辽东栎林群落的土壤温度显著高于其他群落

随着植被恢复

土壤温度变化的范围和峰值均有不同程度的减小

土壤水分有所减少

但并不影响土壤水分随时间变化的总体趋势

不同植被恢复阶段土壤温度和水分呈显著负相关

植被恢复过程中土壤水分有一定的时间稳定性。研究结果可为黄土高原自然植被恢复的有效管理和可持续发展提供科学参考。

Abstract

Soil hydrothermal factor is an important factor affecting the growth and development of crops

especially during the natural vegetation restoration on the Loess Plateau. The dynamic changes and correlations of soil temperature and water in the process of vegetation restoration were studied through long-term monitoring of soil water and temperature in different stages of natural vegetation restoration in the Loess Plateau. The results showed that soil temperature in the grassland community from August to October is significantly higher than other communities

and it is significantly higher in Quercus liaotungens community in November

with the vegetation restoration

the range and the peak of soil temperature decreased with different degree

soil water content decreased but it does not affect the overall varying trend over time

soil temperature and soil water content have significantly negative correlation in the different stages of vegetation restoration

and the soil water content has a certain time stability during the restoration process. The research results provide scientific reference for the effective management and sustainable development of natural vegetation restoration on the Loess Plateau.

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Keywords

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