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亚热带草地水热动态变化及地表能量分配

王恒 张清涛 王志强 吴昕宇

人民珠江2023,Vol.44Issue(12):1-12,53,13.
人民珠江2023,Vol.44Issue(12):1-12,53,13.DOI:10.3969/j.issn.1001-9235.2023.12.001

亚热带草地水热动态变化及地表能量分配

Hydrothermal Dynamics and Surface Energy Allocation in Subtropical Grasslands

王恒 1张清涛 1王志强 1吴昕宇1

作者信息

  • 1. 中山大学土木工程学院,广东 珠海 519082||中山大学华南地区水循环与水安全广东省普通高校重点实验室,广东 广州 510275||广东省海洋土木工程重点实验室,广东 珠海 519082||南方海洋科学与工程广东省实验室,广东 珠海 519082
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摘要

Abstract

Soil hydrothermal changes are an important part of the study of eco-hydrological processes,and studies on soil hydrothermal changes in grasslands in subtropical coastal areas are relatively insufficient.This paper studied the soil hydrothermal changes and surface energy balance of grassland in a subtropical campus area by using field observation data.The results showed that:① Grassland soil moisture is affected differently by rainfall in the wet and dry seasons,with rainfall causing greater soil moisture changes in the dry season than in the wet season.On 20 December,the daily rainfall was 15.2 mm,and the soil moisture change was 0.12 m3/m3 during the study period.On 1 May,the daily rainfall was 120.3 mm,and the soil moisture change was only0.11 m3/m3.②In terms of vertical variation in soil water potential gradient,the zero-pass surface of the soil water potential gradient occurs within 10~30 cm in the wet season and around 50 cm in the dry season.③According to the response of soil moisture to rainfall,soil moisture transport after rainfall in the dry and wet seasons mainly occurs at a soil depth of 0~40 cm.④ The change in soil temperature is greatly influenced by seasonal temperature,and the surface soil temperature gradient is large.In spring and summer,soil temperature decreases with increasing soil depth;in autumn and winter,soil temperature increases with increasing soil depth.⑤ Within two adjacent months,transpiration from grasses is significantly reduced in the wet season relative to the dry season.In terms of energy allocation,although the wet season sees more rainfall and less energy flux,the proportion of latent heat flux is higher,with the proportion of latent heat flux between 0:00 and 6:00 and between 7:00 and 17:00 increasing by 3%and 7%respectively compared with the dry season.This paper examines rainfall and seasonal differences in the hydrothermal dynamics and surface energy of subtropical grasslands,providing information for the study of ecosystems in subtropical coastal zones.

关键词

土壤水势/土壤温度/地表能量/降雨

Key words

soil water potential/soil temperature/surface energy/rainfall

分类

建筑与水利

引用本文复制引用

王恒,张清涛,王志强,吴昕宇..亚热带草地水热动态变化及地表能量分配[J].人民珠江,2023,44(12):1-12,53,13.

基金项目

国家自然科学基金项目(31270748、31470707) (31270748、31470707)

海绵城市建设水系统科学湖北省重点实验室开放基金(武汉大学)(2020-05) (武汉大学)

人民珠江

1001-9235

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