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					  FLUID IDENTIFICATION  LOGGING BASICS The flowmeter tells us how much fluid is 
					moving at any point in a production or injection well, but 
					it tells us nothing about which fluids are present or where 
					each came from. To resolve this, the logging industry has 
					come up with a number of solutions, described later on this 
					page.
 
			
			Portions of this article are from the Schlumberger Glossary, with 
			minor edits and additions from other sources such as PetroWiki.
 
 The term “holdup” appears often in fluid flow literature. It has 
			nothing to do with gun violence or the price of gasoline at the
			service station. It really relates to the fraction of the total flow 
			contributed by each fluid phase, oil, gas, and water.
 
 In multi-phase flow, “holdup” is the fraction of a particular fluid 
			present in an interval of pipe. Each fluid moves at a different 
			speed due to different gravitational forces (fluid density effect) 
			and other factors (viscosity 
			effect), 
			with the heavier phase moving slower, or being more “held up”, than 
			the lighter phase.
 
 The sum of the fluid holdups of the fluids present is unity. The 
			“holdup ratio” is the ratio of the holdups of any two of the fluids. 
			For example, if the water holdup at a particular depth is 0.20, then 
			oil holdup is (1.00 – 0.20) = 0.80 and holdup ratio of oil to water 
			is 0.80 / 0.20 = 4.0.
 
 The holdup of a particular fluid is not the same as the proportion 
			of the total flow rate due to that fluid, also known as its “cut”. 
			To determine in-situ flow rates, it is necessary to measure both 
			holdup and velocity of each fluid.
 
 A “holdup” log is a record of the fractions of different fluids 
			present versus depth in the borehole. Various techniques are used to 
			measure these fractions. The earliest techniques measured the fluid 
			density, using a gradiomanometer, nuclear fluid density log, or the 
			dielectric properties as in the fluid capacitance log.
 
 While these techniques were satisfactory in near-vertical wells with 
			two-phase flow, they were often found to be inadequate in highly 
			deviated and horizontal wells, where flow structures are complex. 
			More recent developments are based on the use of multiple local 
			probes (eg. array capacitance and array spinner imaging tools) to
			detect bubbles of gas, oil, or water, and on a combination of 
			nuclear techniques usually known as three-phase holdup logs.
 
 
  GRADIOMANOMETER
			Introduced in the 
			late 1950s, the gradiomanometer measures the pressure difference 
			between two pressure sensors, placed approximately 2 feet (0.6 m) 
			apart. The pressure difference reflects the average fluid density 
			within that depth interval. The resolution is high, around 0.005 
			g/cc, but the accuracy can be affected by a friction effect, a 
			kinetic effect, and well deviation. The effect of deviation can be 
			corrected, but the sensitivity to holdup is reduced as the deviation 
			increases until it is zero in a horizontal well. 
 If we know or can estimate the density of the individual fluid 
			components (oil, gas, water), we can calculate the relative fraction
			of each fluid present. This allows holdups to be determined, 
			directly in the case of two-phasic flow, and in combination with 
			other measurements for three-phasic flow.
 
 The partitioning equation for a two-phase system is:
 1: HoldUp1 = (DENS - DENS2) / (DENS1 - DENS2)
 2: HoldUp2 = 1 - HoldUp1
 Where:
 HoldUp1 = fraction of fluid 1 at this depth
 HoldUp2 = fraction of fluid 2 at this depth
 DENS = density of fluid mixture (g/cc or kg/m3)
 DENS1 = density of fluid 1 (g/cc or kg/m3)
 DENS2 = density of fluid 2 (g/cc or kg/m3)
 
 With the well shut in and if there is a sump below the perfs, it 
			often contains formation water so water density can be measured 
			directly by the log. Some distance above this, a direct measurement 
			of oil density can be made. Then during stable production, the
			complete log for water holdup can be run.
 
 Numerical Example
 Assume
 DENS1 = downhole water density = 1.110 g/cc
 DENS2 = downhole oil density = 0.710 g/cc
 Composite fluid density = 0.810 g/cc
 
 Water Holdup  = (0.810 - 0.710)/(1.110 - 0.710) = 0.100 / 0.400 = 
			0.25  (or 25%)
 Oil Holdup  = (1.0 - 0.25) = 0.75  (or 75%)
 
 
 
  FLUID CAPACITANCE LOGS This log 
			provides a record of the capability of the fluid passing through a 
			sensor to store electrical charge. Since water has a high dielectric 
			constant, and hence capacitance, the log can distinguish water from 
			oil or gas. The fluid capacitance log can therefore identify water 
			and be scaled in terms of water holdup. However the relation between 
			capacitance and holdup depends strongly on whether the water is the 
			continuous phase, complicating quantitative evaluation.
 
 The log was introduced in the 1960s as the so-called holdup meter. 
			It was mainly used in three-phase flow, or when fluid-density 
			measurements were insufficiently sensitive to water at low holdup, 
			or with heavy oils. Since the late 1980s, other holdup measurements 
			have been preferred.
 
 
 
  NUCLEAR FLUID DENSITY LOG Tool names used by the many service providers are 
			confusing or misleading. Focused gamma ray and unfocused gamma ray 
			logs, for example, do not record a gamma ray log, but they do use a 
			chemical gamma ray source to create a simple uncompensated density 
			log with a very small range of investigation.
 
 These logs measure the density of fluids in a completed well, using 
			a radioactive source of gamma rays and a detector. A cesium 137 or 
			americium 241 source is used to induce Compton scattering, as in the 
			openhole density log, except that the device is unfocused. The count 
			rate at the detector depends primarily on the density of the fluids 
			in the well.
 
 In unfocused  devices, the source and detector are situated so that
			the gamma rays pass outside the tool. The results reflect an average 
			density of all the fluids within the well at that depth. In smaller 
			casings, some formation signal may contaminate the measurement. This 
			type of density log has been used to assess the quality of gravel 
			pack completions.
 
 On some devices, the fluids pass through an open space in the body 
			of the tool within which the measurement is made. The results 
			reflect the density of the fluids passing through the tool. Some 
			people call this type of tool a focused fluid density log since the 
			gamma rays are focused on the wellbore fluid and are not influenced 
			by anything outside the tool body.
 
 Most fluid density logs are scaled in density units (g/cc) but some 
			may have a counts per second (cps) scale. Holdup is calculated as 
			explained for the gradiomanometer,
 
			 Example of a fluid density log using a chemical gamma ray source. 
			Density scale is 0.6 to 1.1 g/cc. Both water and oil densities can 
			be read directly from the log. A natural gamma ray log is in Track1 
			for correlation.
 
 Compared with a gradiomanometer, the nuclear fluid density log is a 
			less direct measurement of density, and has a statistical 
			uncertainty and less resolution, but it is not affected by well 
			deviation, friction, or kinetic effects.
 
 
 
					
					
					 Fluid density (track 1) and spinner survey (tracks 2 and 3). 
					Well flowing 10,000 bpd. Density shows water density in sump 
					below perfs, oil density over perf interval. Spinner shows 
					increasing cumulative production over lower half of perfs.
					The upper half of the perfs may have been ineffective or the 
					reservoir quality is so poor that no flow can be expected. A 
					competent forensic  petrophysical analysis could answer 
					this question and a workover initiated if warranted. 
					Amplified fluid density curve shows slight decrease up to 
					7160 feet indicating some water in the oil below this depth 
					- this is the "water holdup".
 
			
			
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