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					 Formation TEMPERATURE BASICS Formation temperature is an essential piece of knowledge
					needed to calculate water resistivity, which in turn affects 
					the calculation of water saturation and oil and gas in 
					place. It may be measured with a continuous temperature log 
					or during a drill stem or production test. The more usual 
					method is to use the bottom hole temperature (BHT) recorded 
					on the well log heading, along with an assumed surface 
					temperature (SUFT), to create a temperature gradient graph. 
					From this, temperature at any depth may be determined.
 
 1: Grad = (BHT - SUFT) / BHTDEP
 2: FT = SUFT + Grad * DEPTH
 
 Where:
 SUFT = surface temperature for temperature gradient 
					(degrees Fahrenheit or Celsius)
 BHT = bottom hole temperature (degrees Fahrenheit or 
					Celsius)
 Grad = temperature gradient (degrees F / foot or degrees C 
					\ meter)
 BHTDEP = depth at which BHT was measured (feet or meters)
 DEPTH = mid-point depth of reservoir (feet or meters)
 FT = formation temperature (degrees Fahrenheit or Celsius)
 
 Many basins have local “hot spots”, with temperature 
					gradients much higher than the basin average. Water sature 
					will be too high and oil and gas inc place will be too low 
					if a low temperature gradient or low formation temperature 
					is used. instead of the correct one.
 
 
 
 
  ESTIMATING
				SURFACE TEMPERATURE Temperature
				measurements specific to your area of interest are going to
					be sparse and you will have to do some searching for useful data.
				The map below gives a good idea of what to use for surface
				temperature (SUFT).
 
				
			 Mean Annual Surface Temperature Map for North America - degrees F
 The 40 deg F contour follows roughly along the US-Canada border
			except along the coast lines.
 Contour interval is 5 deg F.
 
			
			
			 ESTIMATING 
			FORMATION TEMPERATURES Temperature 
			versus depth data from log headings can be plotted to estimate a 
			best fit temperature gradient line. It doesn't have to be a straight 
			line. See representative graphs below. In areas with sparse data, 
			use the temperature gradient maps supplied below.
 
				 Typical Depth - Temperature profiles. Create your own by
				best fit of BHT vs BHTDEP from data on log
 headings or DST reports.
 
			 Temperature gradient for USA -
			degrees Celsius per 1000 meters,
 North American Heat Floe Map
			(3 MB)    
			Legible Legend for NA Map
 
			 Temperature at 5000 meters for
			Australia
 
					
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