C-11653 (Biosolids Project)
Land Application of Residuals and Chicken Manure in the Lake Okeechobee Watershed: Phosphorus Considerations

Field Test Methods
Temperature
Standard Method (SM) 2550A. and 2550B.

2550 A. Introduction

Temperature readings are used in the calculation of various forms of alkalinity, in studies of saturation and stability with respect to calcium carbonate, in the calculation of salinity, and in general laboratory operations. In limnological studies, water temperatures as a function of depth often are required. Elevated temperatures resulting from discharges of heated water may have significant ecological impact. Identification of source of water supply, such as deep wells, often is possible by temperature measurements alone. Industrial plants often require data on water temperature for process use or heat-transmission calculations.

* Approved by Standard Methods Committee, 1988.

 2550 B. Laboratory and Field Methods

 1.  Laboratory and Other Non-Depth Temperature Measurements

Normally, temperature measurements may be made with any good mercury-filled Celsius thermometer. As a minimum, the thermometer should have a scale marked for every 0.1°C, with markings etched on the capillary glass. The thermometer should have a minimal thermal capacity to permit rapid equilibration. Periodically check the thermometer against a precision thermometer certified by the National Institute of Standards and Technology (NIST, formerly National Bureau of Standards)* that is used with its certificate and correction chart. For field operations use a thermometer having a metal case to prevent breakage.

2. Depth Temperature Measurements

Depth temperature required for limnological studies may be measured with a reversing thermometer, thermophone, or thermistor. The thermistor is most convenient and accurate; however, higher cost may preclude its use. Calibrate any temperature measurement devices with a NIST-certified thermometer before field use. Make readings with the thermometer or device immersed in water long enough to permit complete equilibration. Report results to the nearest 0.1 or 1.0°C, depending on need.

The thermometer commonly used for depth measurements is of the reversing type. It often is mounted on the sample collection apparatus so that a water sample may be obtained simultaneously. Correct readings of reversing thermometers for changes due to differences between temperature at reversal and temperature at time of reading. Calculate as follows:

       DT = [ (T’ – t) (T’ + V₀) ] x  [ 1 + (T’ – t) (T’ + V₀) ] + L
                              K                                    K

where:

DT = correction to be added algebraically to uncorrected reading,
T' = uncorrected reading at reversal,
t = temperature at which thermometer is read,
V₀ = volume of small bulb end of capillary up to O'C graduation,
K = constant depending on relative thermal expansion of mercury and glass (usual value of K = 6100), and
L = calibration correction of thermometer depending on T'.

If series observations are made, it is con- venient to prepare graphs for a thermometer to obtain DT from any values of T' and t.

  * Some commercial thermometers may be as much as 3°C in error.

3. Bibliography

 WARREN, H.F'. & G.C. WHIPPLE. 1895. The thermophone-A new instrument for determining temperatures. Mass. Inst. Technol. Quart. 8-125.

SVERDRUP, H.V., M.W. JOHNSON & R.H. FLEMING. 1942. The Oceans. Prentice- Hall, Inc., Englewood Cliffs, N.J.

AMERICAN SOCIETY FOR TESTING AND MATERIALS. 1949. Standard Specifications for ASTM Thermometers. No. El-58, ASTM, Philadelphia, Pa.

REE, W.R. 1953. Thermistors for depth thermometry. J .Amer. Water Works,Assoc. 45-259.

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Last update: May 18, 2003 by Stephane Grounauer