Abstract
采用灰色关联分析方法研究自然因素对和田绿洲地下水埋深的影响, 并建立多元线性回归模型进行检验。结果表明, 气温、蒸发是地下水埋深的两个最重要的影响因子, 埋深随蒸发增加、气温升高而增大。出山口径流(主要为冰雪融水)对地下水埋深的影响仅次于气温和蒸发, 埋深随径流增大而逐渐减小, 约有1~2个月的滞时。风速、水温和湿度对地下水埋深的影响相对较小, 降水与地下水埋深的关系不太明显。影响因子与埋深的多元线性回归模型的拟合精度较高, 且通过了置信水平<i>α</i> = 0.01的显著性检验。
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.