Hydraulic Conductivity Measurements in the Unsaturated Zone Using Improved Well Analyses

Groundwater Monitoring & Remediation

Volumn 9, Issue 3, 1989, Pages 184-193

  Elrick, D E ^a   Reynolds, W D ^a   Tan, K A ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

CONSTANT HEAD WELL PERMEAMETER TECHNIQUE; GROUNDWATER FLOW; HYDRAULIC CONDUCTIVITY MEASUREMENT; UNSATURATED ZONE; WELL ANALYSIS;

EID: 0024783228     PISSN: 10693629     EISSN: 17456592     Source Type: Journal    
DOI: 10.1111/j.1745-6592.1989.tb01162.x     Document Type: Article

References (30)

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8. Physical theory for capillary flow phenomena
9. Approximate analysis of the borehole permeameter in unsaturated soil
10. In situ measurement of field‐saturated hydraulic conductivity, sorptivity, and the α‐parameter using the Guelph permeameter
11. A method for simultaneous in situ measurement in the vadose zone of field‐saturated hydraulic conductivity, sorptivity, and the conductivity‐pressure head relationship
12. A laboratory and numerical assessment of the Guelph Permeameter method
13. A reexamination of the constant head well permeameter method for measuring saturated hydraulic conductivity above the water table
14. The constant head well permeameter. Effect on unsaturated flow
15. Watershed physics: soil variability criteria
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17. Analysis of water flow from cylindrical macropores
18. Vadose zone permeability tests: summary
19. Regression models for hydraulic conductivity and field test of the borehole permeameter
20. Vadose zone characterization of low‐permeability sediments using field permeameters
21. Re‐evaluation of the well permeameter as a field method for measuring hydraulic conductivity
22. The variation of in‐situ measured soil water properties within soil map units
23. A closed‐form equation for predicting the hydraulic conductivity of unsaturated soils
24. Spatial variability of soil physical properties in the field
25. Use of sorptivity to determine field soil hydraulic properties
26. Macroscopic and microscopic capillary length and time scales from field infiltration