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https://hdl.handle.net/11681/9094Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Black, Patrick B. | - |
| dc.date.accessioned | 2016-06-20T13:40:14Z | - |
| dc.date.available | 2016-06-20T13:40:14Z | - |
| dc.date.issued | 1990-05 | - |
| dc.identifier.uri | http://hdl.handle.net/11681/9094 | - |
| dc.description | CRREL Report | - |
| dc.description | Abstract: Empirically determined data on changes in unfrozen water content occurring as result of changes in the state of ice and water in soil are discussed with reference to the changes in soil-water retention data for ice-free soil. The similarity between the two types of data is developed. The Brooks and Corey, van Genuchten and Gardner equations are then shown to be applicable to describing unfrozen water content data. These three functions are then used in the model of Mualem and the relative hydraulic conductivity of frozen soil is predicted. | - |
| dc.publisher | Cold Regions Research and Engineering Laboratory (U.S.) | - |
| dc.publisher | Engineer Research and Development Center (U.S.) | - |
| dc.relation | http://acwc.sdp.sirsi.net/client/en_US/search/asset/1001230 | - |
| dc.relation.ispartofseries | CRREL report ; 90-5. | - |
| dc.rights | Approved for public release; distribution is unlimited. | - |
| dc.source | This Digital Resource was created from scans of the Print Resource | - |
| dc.subject | Frozen soil | - |
| dc.subject | Frozen ground | - |
| dc.subject | Hydraulic conductivity | - |
| dc.subject | Unfrozen water | - |
| dc.subject | Soil permeability | - |
| dc.title | Three functions that model empirically measured unfrozen water content data and predict relative hydraulic conductivity | - |
| dc.type | Report | en_US |
| Appears in Collections: | CRREL Report | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| CRREL-90-5.pdf | 277.99 kB | Adobe PDF |  View/Open |