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The '''Amott test''' is one of the most widely used empirical [[wettability]] measurements for reservoir [[Core sample|cores]] in [[petroleum engineering]]. The method combines two spontaneous [[imbibition]] measurements and two forced displacement measurements. This test defines two different indices: the Amott water index (<math>I_w</math>) and the Amott oil index (<math>I_o</math>).


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==Amott–Harvey index==
The two Amott indices are often combined to give the '''Amott–Harvey index'''. It is a number between -1 and 1 describing wettability of a rock in drainage processes. It is defined as:
:<math>AI=I_w-I_o</math>
[[Image:Amott-Harvey_Index_calculation.png|thumb|300px|right|Figure 1: Amott–Harvey index and USBM number calculation.]]
These two indices are obtained from [[special core analysis]] (SCAL) experiments ([[porous plate]] or [[centrifuge]]) by plotting the capillary pressure curve as a function of the water saturation as shown on figure 1:
:<math>I_w=\frac{S_{spw}-S_{cw}}{1-S_{cw}-S_{or}}</math>
with <math>S_{spw}</math> is the water saturation for a zero capillary pressure during the imbibition process, <math>S_{cw}</math> is the irreducible water saturation and <math>S_{or}</math> is the residual oil saturation after imbibition.
:<math>I_o=\frac{S_{spo}-S_{or}}{1-S_{cw}-S_{or}}</math>
with <math>S_{spo}</math> is the oil saturation for a zero capillary pressure during the [[secondary drainage]] process, <math>S_{cw}</math> is the irreducible water saturation and <math>S_{or}</math> is the residual non-wetting phase saturation after imbibition.
 
A rock is defined as:
* Water wet when the Amott–Harvey index is between 0.3 and 1,  
* Weakly water wet when the Amott–Harvey index is between 0 and 0.3,
* Weakly oil wet when the Amott–Harvey index is between -0.3 and 0,
* Oil wet when the Amott–Harvey index is between -1 and -0.3.
 
==See also==
* [[USBM index]] - an alternative wettability index
* [[Relative permeability]]
* [[Multiphase flow]]
* [[Capillary pressure]]
* [[Leverett J-function]]
* [[Imbibition]]
 
==External links==
* http://www.jgmaas.com/scores/facts.html
 
==References==
* Dake, L.P., "Fundamentals of Reservoir Engineering", Elsevier Scientific Publishing Company, Amsterdam, 1977.
* Amott, E., "Observations relating to the wettability of porous rock", Trans. AIME 219, pp. 156–162, 1959.
[[Category:Fluid dynamics]]
 
 
{{fluiddynamics-stub}}

Latest revision as of 05:01, 23 January 2014

The Amott test is one of the most widely used empirical wettability measurements for reservoir cores in petroleum engineering. The method combines two spontaneous imbibition measurements and two forced displacement measurements. This test defines two different indices: the Amott water index () and the Amott oil index ().

Amott–Harvey index

The two Amott indices are often combined to give the Amott–Harvey index. It is a number between -1 and 1 describing wettability of a rock in drainage processes. It is defined as:

Figure 1: Amott–Harvey index and USBM number calculation.

These two indices are obtained from special core analysis (SCAL) experiments (porous plate or centrifuge) by plotting the capillary pressure curve as a function of the water saturation as shown on figure 1:

with is the water saturation for a zero capillary pressure during the imbibition process, is the irreducible water saturation and is the residual oil saturation after imbibition.

with is the oil saturation for a zero capillary pressure during the secondary drainage process, is the irreducible water saturation and is the residual non-wetting phase saturation after imbibition.

A rock is defined as:

  • Water wet when the Amott–Harvey index is between 0.3 and 1,
  • Weakly water wet when the Amott–Harvey index is between 0 and 0.3,
  • Weakly oil wet when the Amott–Harvey index is between -0.3 and 0,
  • Oil wet when the Amott–Harvey index is between -1 and -0.3.

See also

External links

References

  • Dake, L.P., "Fundamentals of Reservoir Engineering", Elsevier Scientific Publishing Company, Amsterdam, 1977.
  • Amott, E., "Observations relating to the wettability of porous rock", Trans. AIME 219, pp. 156–162, 1959.


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