Examining the potentials and limitations of using temperature tracing to infer water flux through unsaturated soils

Melissa Clutter, Paul A Ferre

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

Irrigation agriculture is the primary consumer of water worldwide. Because groundwater resources are being depleted, there is an increasing need to measure subsurface flux to quantify consumptive use and return flow. This study used HYDRUS-1D to simulate one-dimensional vertical movement of water and heat. Temperature time series were analyzed for different materials, depths, and applied fluxes to understand the limitations of temperature methods for monitoring steady-state water flux under unsaturated conditions. The conditions used in this analysis were intended to explore the minimum standards needed for unsaturated, steady-state flux estimation. If these conditions cannot be met, then it is unnecessary to look at more challenging conditions (e.g., heterogeneity, transient flux, and unknown hydraulic and thermal properties). Previous work has suggested that there is a minimum flux that is measurable with temperature methods. The low saturated hydraulic conductivities of fine-grained materials limit the applicability of temperature methods to high fluxes that lead to near-saturated conditions for these materials. Although coarser soils have higher hydraulic conductivities, thermal diffusivity increases significantly with decreasing water content and may still complicate flux measurements for unsaturated conditions. As a result, we conclude that temperature-based methods in unsaturated conditions will most likely fail even with the most simplifying assumptions for most soil types. Therefore temperature methods should be restricted to monitoring steady-state fluxes in coarse soils and/or conditions near saturation.

Original languageEnglish (US)
Article number170181
JournalVadose Zone Journal
Volume17
Issue number1
DOIs
StatePublished - Feb 1 2018
Externally publishedYes

Fingerprint

unsaturated conditions
soil
temperature
water
hydraulic conductivity
thermal diffusivity
saturated conditions
methodology
monitoring
vertical movement
saturated hydraulic conductivity
thermal properties
drainage water
flux measurement
groundwater resource
diffusivity
soil type
soil types
time series analysis
fluid mechanics

ASJC Scopus subject areas

  • Soil Science

Cite this

Examining the potentials and limitations of using temperature tracing to infer water flux through unsaturated soils. / Clutter, Melissa; Ferre, Paul A.

In: Vadose Zone Journal, Vol. 17, No. 1, 170181, 01.02.2018.

Research output: Contribution to journalArticle

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