干旱区研究 ›› 2020, Vol. 37 ›› Issue (1): 116-125.
孙海涛1,2 ,陈亚鹏1,2*,陈亚宁1,张颖1,2,何振磊1,2
收稿日期:
2019-04-12
修回日期:
2019-05-28
出版日期:
2020-01-15
发布日期:
2020-01-14
通讯作者:
陈亚鹏
作者简介:
孙海涛(1991-),男,硕士研究生,研究方向为干旱区地下水与生态水文过程.E-mail: sunhaitao16@mails.ucas.ac.cn
基金资助:
SUN Hai-tao1, 2, CHEN Ya-peng1, 2,
CHEN Ya-ning1, ZHANG Ying1, 2, HE Zhen-lei1, 2
Received:
2019-04-12
Revised:
2019-05-28
Online:
2020-01-15
Published:
2020-01-14
摘要:
通过对塔里木河下游4个观测点地下水位的监测和地下水蒸散发的估算,分析荒漠河岸林地下水位月和日的波动、地下水蒸散发(ETg)的时空变化及其主要影响因素。结果表明:① 在生态输水前(7月21日至8月12日),4个观测点地下水位呈整体下降趋势;而生态输水后,水位保持稳定上升趋势。在整个观测期内,地下水位都表现出明显的昼夜波动现象。② ETg 均呈现出单峰变化特征,8:00开始快速增加,在12:00—16:00维持在一个较高水平上,18:00以后快速下降,最高值出现在当地时间14:00。③ ETg随着植被类型、覆盖度的不同而存在显著差异,同时又受地下水位埋深的影响。④ 太阳辐射、温度和饱和水气压差是影响塔里木河下游地下水蒸散发日变化的主要因素,风速对其无显著影响。
孙海涛, 陈亚鹏, 陈亚宁, 张颖, 何振磊. 塔里木河下游荒漠河岸林地下水蒸散发[J]. 干旱区研究, 2020, 37(1): 116-125.
SUN Hai-tao, CHEN Ya-peng, CHEN Ya-ning, ZHANG Ying, HE Zhen-lei. Groundwater Evapotranspiration in Desert Riparian Forest in the Lower Reaches of the Tarim River[J]. Arid Zone Research, 2020, 37(1): 116-125.
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