THE MECHANISM BY WHICH WATER MOVES THROUGH A POROUS MATERIAL SUBJECTED TO A TEMPERATURE GRADIENT: 2. SALT TRACER AND STREAMING POTENTIAL TO DETECT FLOW IN THE LIQUID PHASE KUZMAK, J. M.; SEREDA, P. J. KUZMAK, J. M.; SEREDA, P. J. Less Soil Science. 84(5):419-422, November 1957. Favorites PDF Get Content & Permissions Buy
THE MECHANISM BY WHICH WATER MOVES THROUGH A POROUS MATERIAL SUBJECTED TO A TEMPERATURE GRADIENT: I. INTRODUCTION OF A VAPOR GAP INTO A SATURATED SYSTEM KUZMAK, J. M.; SEREDA, P. J. KUZMAK, J. M.; SEREDA, P. J. Less Soil Science. 84(4):291-300, October 1957. Favorites PDF Get Content & Permissions Buy
