From: Peter Waldispuehl ("peter.waldispuehl") To: sowacs@aqua.ccwr.ac.za Date: Monday, July 29, 1996 4:10 pm Subject: monitoring - field experience Hello, I'm employed for a project called "Longterm Forest EcosystemResearch" (LTFER) and I have joined SoWaCS a few days ago. I am responsiblefor soil physics and soil water studies on the Swiss LTFER-plots. Thisincludes water balance quantification, determination of soil hydraulicproperties and water balance modelling. Because I have no field experience, I'm very interested inexchanging information with scientists doing field monitoring. I started my work a few weeks ago. My first goal now is thedetermination of the (field) water characteristic function for some of theplots. 1) What kind of instruments (with respect to accuracy, samplevolume, resolution, ...) might be advisable for this kind of task. 2) Topp and Davis (1985) describe a vertical installation of TDRrods to get less disturbance than with horizontal measurements (no pitnecessary). Does this work with rods of about 1 m length in any soil?Experiences with this kind of installation? 3) Alpine plots pose a special problem: installation andmeasurements are disturbed by a very high stone content. Any solutions? Is therefor example a possibility to correct TDR-readings for stone content? Whatabout other kind of soil moisture sensors? 4) What are the experiences with FDR sensors so far? 5) Recommendable literature on the determination of field water characteristic function? Thanks for any hints! Literature: Topp, G. C. and J. L. Davis. 1985. Measurement of soilwater content using time-domain reflectometry (TDR): a field evaluation.Soil Sci. Soc. Am. J. 49:19-24 ################################################################# Peter Waldispuehl Soil Physics (Long-term Forest Ecosystem Research) Swiss Federal Institute for Forest, Snow and Landscape Research Zuercherstr. 111, CH-8903 Birmensdorf ZH, Switzerland e-mail peter.waldispuehl@wsl.ch Phone ++41 1 739 25 92 Fax ++41 1 739 22 15 #################################################################