Development of an Experimental Apparatus for Studying High-Temperature Heat and Mass Transfer in Soils
Bibliographic record
Abstract
The objective of this study was to design and build an experimental apparatus for studying heat and moisture transport phenomena in soils at temperatures greater than 40°C up to 90°C. An experimental soil cell was designed and constructed for experimental studies of one-dimensional heat and moisture transfer within a vertical soil column. The interference effect between two proximate TDR probes was examined for three types of soils and it was found that parallel TDR probes can interfere with each other if the distance between them is around 1 cm. Also, for the samples with higher water contents, the effect of interference on the electromagnetic waveform signals is more prominent, which can result in 15% uncertainty in the measurement of water content. Through the numerical study, four stages of design analysis were carried out to eventually reach a satisfactory design which was deemed to meet the research objective, i.e. less than 5% variation of heat fluxes in the radial direction along the soil cell. The experimental assessment of the final soil cell was first performed using dry Matilda soil. The temperature profile along the soil cell deviated from the linear temperature profile by 18.6% when the temperature level and gradient was high at 82.6°C and 90°C/m, respectively. At this condition, the difference of heat fluxes between the top and bottom heat flux meters was recorded to be 34%. This case is the worst case due to the low thermal conductivity of the dry soil. The experimental assessment of the final soil cell was also done for a wet Matilda soil at a degree of saturation of about 65%. The temperature profile along the soil cell had a maximum deviation of 7.7% from the linear temperature profile even when the temperature level of the soil cell was high at 82.1°C. At this condition, the difference of heat fluxes between the top and bottom heat flux meters was recorded to be 4.2%. After the reliability of the apparatus was assessed, nine cases of the wet soil were studied. The results show that the temperature gradient is the main driving force to cause moisture migration.
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How this classification was reachedexpand
Full frame distilled prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.000 | 0.000 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one teacher head, not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".