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NOTE: To get off this list, send email to majordomo@aqua.ccwr.ac.za with the body of the message containing the line: unsubscribe sowacs Elizabeth, The relationship between the humidity above a solution and the thermodynamic potential of the solution is given by ht = (RT/Mg) ln (H) where ht = the thermodynamic potential (in cm of water) R = ideal gas constant T = absolute temperature M = molar weight of water g = acceleration of gravity H = relative humidity produce by the solution the units of ht are a function of the units on the right hand side. You can use any solution you want. Some have used various concentrations of sulfuric acid solutions, but they are a little bit of a hassle since the solutions must be refreshed as water evaporates or condenses changing the concentration with it. An article in Ecology 41:233 (1960) published a long list of salts, whose saturated solutions produce a range of humilities. Saturated salt solutions have the advantage in that as long as the solid salt is present, the solution will maintain a constant humidity as water is exchanged with the atmosphere. Two words of caution. 1. Your need a constant temperature within 1 degree C. 2. It takes a long time to reach equilibrium via vapor transport. Be prepared to wait one week or even a month. You can however speed up the process by placing the solution and sample inside a vacuum chamber. (Vapor diffusion coefficients are inversely proportional to the total pressure.) Here are the solutions I use and their H and ht at 22.5 C Salt H ht (cm of H20) ZnCl2 0.100 -3.20 x 10^6 MgCl2 0.328 -1.55 x 10^6 K2CO3 0.436 -1.14 x 10^6 Mg(NO3)2 0.542 -8.51 x 10^5 NaNO2 0.649 -6.00 x 10^5 NaCl 0.758 -3.85 x 10^5 KCl 0.850 -2.26 x 10^5 KNO3 0.931 -9.93 x 10^4 K(H2PO4)2 0.963 -5.24 x 10^4 K2Cr207 0.980 -2.82 x 10^4 Good luck. Glenn Brown Associate Professor Biosystems Engineering Oklahoma State University Stillwater, OK 74078 (405) 744-8425 gbrown@okstate.edu -----Original Message----- From: owner-sowacs@aqua.ccwr.ac.za <owner-sowacs@aqua.ccwr.ac.za> To: gbrown@ceat.okstate.edu <gbrown@ceat.okstate.edu> Date: Thursday, January 25, 2001 9:23 AM Subject: Thermal Conductivity Sensors Bruce: > >I am going to be calibrating some of the Campbell Scientific 229 sensors. > I am going to use pressure from 0-400 kPa but I would like to calibrate >at a higher kPa. I read somewhere that letting the sensors "hang" in a >jar containing a solution of potassium sulfate at 20 degrees Celcius will >give an equivalent total suction of 4120 kPa. Do you know of a solution >(and temperature) that might give an equivalent total suction between 400 >and 4120 kPa? I would really appreciate the input. > Elizabeth A. Garven > 125B-105th Street >East > >Saskatoon, Saskatchewan > >CANADA > >Phone: (306) 955-3218 > ><<mailto:eag-okc@attcanada.ca>eag-okc@attcanada.ca