期刊论文详细信息
JOURNAL OF HYDROLOGY 卷:582
Comparison of negative skewed space fractional models with time nonlocal approaches for stream solute transport modeling
Article
Sun, Liwei1,2  Qiu, Han3  Niu, Jie1,2  Hu, Bill X.1,2  Kelly, James F.4  Bolster, Diogo5  Phanikumar, Mantha S.6 
[1] Jinan Univ, Inst Groundwater & Earth Sci, Guangzhou 510632, Peoples R China
[2] Green Dev Inst Zhaoqing, Zhaoqing 526000, Peoples R China
[3] Pacific Northwest Natl Lab, Joint Global Change Res Inst, College Pk, MD 20740 USA
[4] US Naval Res Lab, Washington, DC 20375 USA
[5] Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA
[6] Michigan State Univ, Dept Civil & Environm Engn, E Lansing, MI 48824 USA
关键词: Transient storage;    Fractional derivative;    Hyporheic zone;    Continuous time random walk;   
DOI  :  10.1016/j.jhydrol.2019.124504
来源: Elsevier
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【 摘 要 】

Continuous time random walks (CTRW), multi-rate mass transfer (MRMT), and fractional advection-dispersion equations (FADEs) are three promising models of anomalous transport as commonly found in natural streams. Although these paradigms are mathematically related, understanding their advantages and limitations poses a challenge for model selection. In this paper, we quantitatively evaluate the advection-dispersion equation (ADE), fractional-mobile-immobile (FMIM), fractional-in-space ADE (sFADE), fractional in space transient storage (FSTS), truncated time-fractional model (TTFM), and CTRW models with truncated power-law waiting time distribution (CTRW-TPL) by fitting them first to synthetic data. We then applied these models to observations from tracer experiments conducted in several rivers. Based on the extensive analysis, we conclude that the performance of the FSTS model (in particular, the model with negative skewness beta = -1) is comparable or superior to the other nonlocal models evaluated in the paper, therefore, the model represents an alternative to existing models for simulating stream solute transport for spatially-homogeneous flows.

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