2015年塔克拉玛干沙漠腹地达理雅博依天然绿洲浅层地温变化特征

王金花; 张峰; 师庆东

doi:10.13568/j.cnki.651094.2019.03.002

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2015年塔克拉玛干沙漠腹地达理雅博依天然绿洲浅层地温变化特征

专栏:绿洲生态学 | 更新时间：2026-01-21

- 2015年塔克拉玛干沙漠腹地达理雅博依天然绿洲浅层地温变化特征
- 2015年塔克拉玛干沙漠腹地达理雅博依天然绿洲浅层地温变化特征
- 新疆大学学报（自然科学版中英文） 2019年36卷第3期页码：260-266
- 作者机构：
  
  新疆大学绿洲生态教育部重点实验室
- 作者简介：
- 基金信息：
  
  国家自然科学基金新疆联合基金项目(U1178303)和(U1703237)共同资助
- DOI：10.13568/j.cnki.651094.2019.03.002
  中图分类号： P423.3
- 纸质出版：2019
- 稿件说明：
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[1]王金花,张峰,师庆东.2015年塔克拉玛干沙漠腹地达理雅博依天然绿洲浅层地温变化特征[J].新疆大学学报(自然科学版),2019,36(03):260-266.
[1]王金花,张峰,师庆东.2015年塔克拉玛干沙漠腹地达理雅博依天然绿洲浅层地温变化特征[J].新疆大学学报(自然科学版),2019,36(03):260-266. DOI： 10.13568/j.cnki.651094.2019.03.002.

DOI：10.13568/j.cnki.651094.2019.03.002.

摘要

地温为地-气系统研究的一个重要参数.克里雅河尾闾达理雅博依为塔里木盆地一典型的原始荒漠绿洲

对天然绿洲生态过程、形成机理及演化研究极具意义

而该地区地温等相关气象数据却极少发表.本文以达理雅博依所建首台区域气象站所采集的地温数据为基础

分析了2015年1月至2016年4月5～20 cm各浅层土壤温度的日变化及季节变化特征.结果表明:各层地温月平均值年内变化趋势较为一致

呈正弦曲线变化

7月为峰

1月为谷.各浅层地温月变幅随深度增加而减小

且波动幅度夏季最大

冬季最小.各层地温年平均值为14.8℃

低于大致同纬度的塔中气象站(16℃左右)

且地温年变化升降较塔中相对缓和

显示绿洲与沙漠环境存在差异.各层土壤日变化亦基本呈正弦变化

随深度增加

日最高和最低值位相逐渐滞后

振幅亦随之减小;达理雅博依7月5 cm地温日最大值和最低值出现时刻明显晚于塔中

反映了二者土壤热容的不同.日最高值波动幅度高于日最低值

夏半年波动幅度又显著高于冬半年.

Abstract

Ground temperature is an important parameter for research on the Earth-atmosphere system. Daliyaboyi at the lower reaches of the Keriya River is a typical primitive desert oasis in the Tarim Basin that is important for research on ecological processes

formation mechanisms

and evolution research of natural oases

but relevant meteorological data of the ground temperature is rarely published. Based on the ground temperature data(5-20 cm depths) obtained at the first regional meteorological station at Daliyaboyi for 2015-2016

the characteristics of daily and seasonal variations in the ground temperature have been analyzed. The results show that the intra-annual variation trends of the monthly mean value for each layer of ground temperature are consistent

which are all a sine curve

July is the peak and January is the lowest ebb. The variation in amplitude of the monthly mean value for the ground temperature at each layer decreases as the depth increases

the amplitude of fluctuation is the greatest in summer and the least in winter. Meanwhile

the annual mean ground temperature at all depths(about 14.8 ℃)is less than at Tazhong station(about 16 ℃) and the temperature fluctuation is relatively gentle

which shows the difference in environments between the oasis and the desert. Similar to changes within the year

diurnal variation at all depths of ground temperature showed a sinusoidal variation

the daily maximum and minimum values underwent phase lag as the depth increased and the amplitude decreased accordingly. Compared to Tazhong in July

the moments for the maximum and minimum value of the ground temperature at 5 cm appeared later

which was caused by their different soil thermal capacities. The fluctuation of the daily maximum value was larger than the minimum; Meanwhile

the fluctuation in the summer half of the year was larger than for the winter half of the year.

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