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避免异参同效的抽水井表皮层溶质运移方程推导

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抽水井表皮层溶质运移控制方程受到异参同效的影响,存在参数估计的多解性问题.提出一个新的抽水井表皮层溶质运移方程(新瞬态Robin边界条件),并以径向收敛示踪试验为例构建其溶质运移模型.当抽水井为完整井时,通过拉普拉斯变换和有限傅立叶余弦变换得到模型的解析解;当抽水井为非完整井时,应用有限元法构建数值解.结果表明,表皮层溶质运移控制方程导致所估计的表皮层宽度(w)和形成层垂向弥散度(αz)是在0.5 m≤w≤1.0 m和0.08 m≤αz≤0.10 m范围内的任意组合,偏离实际值.反之,当表皮层佩克莱数(w和表皮层径向弥散度的比值)小于1时,新瞬态Robin边界条件能够准确反映表皮层的影响,消除w与αz的多解性.参数估计值(w=0.31 m、αz=0.17 m)唯一,接近实际值.新模型已成功用于野外试验.
Derivation of Solute Transport Equation for the Skin of an Extraction Well without Equifinality
The governing equation of solute transport in the well skin produces multiple parameter estimates because of the equifinality of modeling radially convergent tracer tests.A new transport equation for the skin of an extraction well(i.e.,a new transient Robin boundary condition)is proposed.A new analytical model was developed to test a fully penetrating extraction well.The analytical solution of the model was obtained using the Laplace transform and finite Fourier cosine transform.A finite element solution was acquired for the test in a partially penetrating extraction well.Results suggest the skin governing equation produces the estimates of the skin width w and formation vertical dispersivity αz are arbitrary values chosen from the ranges of 0.5 m≤w≤1 m and 0.08 m≤αz≤0.1 m.These ranges exclude the default values.In contrast,the new Robin boundary condition accurately reflects the skin effect when the Peclet number,defined as the ratio of w to the longitudinal dispersivity of the skin,is less than 1.The present solution relying on this boundary condition predicts the single optimal estimates of w and αz.The estimates(w=0.31 m,αz=0.17 m)approach their default values.The present solution applies to field tests.

Radially convergent tracer testEquifinalityTransient Robin boundary conditionAnalytical solutionFinite element solution

蒯沐钦、黄璟胜、童晨晨、王晨、肖烨熙

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河海大学水文水资源学院,江苏 南京 210098

径向收敛示踪试验 异参同效 瞬态Robin边界条件 解析解 有限元解

国家自然科学基金国家自然科学基金

5237906252079042

2024

地球科学进展
中国科学院资源环境科学信息中心 国家自然科学基金委员会地球科学部 中国科学院资源环境科学与技术局

地球科学进展

CSTPCD北大核心
影响因子:2.045
ISSN:1001-8166
年,卷(期):2024.39(3)
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