Bu Parvita,
Koreksi overburden seharusnya dilakukan. Kalau kata sumber yg bisa dipercaya 
sih "Overburden correction can reduce the porosity from 0.5-1.0 p.u. (ratio: 
0.90-0.97):.jadi setelah koreksi, porositas-nya bisa 0.9-0.97 kali dari awalnya.
Archie Formula:(Sw^n)= FF(Rw/Rt)Jika Sw= 100% maka Ro=RtFormation 
Factor=a/(porositas^m)=Ro/RwResistivity Index=RI=1/(Sw^n)=Rt/R0
Dari rumus di-atas sudah jelas bahwa porositas cukup menentukan dalam 
Electrical Measurement CCAL.
Dari sumber yang bisa dipercaya: nilai m setelah koreksi overburden= nilai m 
ambient+0.05 sampai nilai m ambient+0.1 (ratio 1.05-1.1). jadi setelah 
dikoreksi akan didapatkan nilai m yang lebih besar.
Sumber kesalahan dari kalkulasi porositas CCAL: pencucian, 
pengeringan,pengukuran reservoir stress, jenis texture, 
Representavity/homogeneity. Pengeringan pada suju 80 degC seringkali 
menyebabkan mineral lempung rusak (shale collapse) sehingga menambah nilai 
porositas. Disarankan di suhu 60 degC saja, nggak usah panas2.

Ketidakpastian nilai m:- Error porositas versus error m- m overburden versus m 
ambient (nilai m meningkat sebanding dengan porositas)- Plugs anisotropy 
(bedding, fissures, conductive minerals, dll) 


Ketidakpastian nilai m:-Plugs harus di_de-saturated- Jangan pakai plugs apabila 
Sw mini > 40-50%.- Error pada porositas --> error pada Sw --> eror pada nilai 
n- Hysteresis on RI ; Sheath effect on Pc and RI yang akan menghasilkan 
artificial porositas hingga 2 kali lipat (Swanson, 1985)

Berikut ada rujukan tambahan:----FORMATION RESISTIVITY MEASUREMENTS(Core Lab, 
2007, Application of Core Analysis In Reservoir Description & Characterisation)
MethodsResistance is measured and converted to resistivity of the 100% or 
partially brine-saturated sample. Tests normally made at ambient temperature 
and net overburden pressure can be simulated.---Effect of Overburden Pressure 
on Resistivity(Buku: Torsæter & Abtahi, 2003, RESERVOIR ENGINEERING LABORATORY 
WORK BOOK, Norwegian University of Science and Technology)Confinement or 
overburden pressure may cause a significant increase in resistivity. 
Thisusually occurs in rocks that are not well cemented and in lower porosity 
rocks. Archie, asmentioned before, reported results of correlating laboratory 
measurements of formationfactor with porosity in the formF m _6.11_ __ _Wyllie 
investigated the influence of particle size and cementation factor on the 
formationfactor of a variety of materials. He concluded that the cemented 
aggregates exhibit agreater change in formation factor with a change in 
porosity than the unconsolidatedaggregates. Then, the general
 form of the relation between formation factor and porosityshould beF a m 
_6.12_ __ _where m is a constant depending on cementation and a a constant 
controlled by theporosity of the unconsolidated matrix prior to cementation. 


Salam,YES

Sent from my BlackBery® wireline handheldSinyal Bagus Indonesia, Nyambung 
Teruuusss...!

--- On Wed, 6/15/11, Parvita Siregar <[email protected]> 
wrote:

From: Parvita Siregar <[email protected]>
Subject: [iagi-net-l] Formation resistivity factor (a, m, n)
To: "[email protected]" <[email protected]>
Date: Wednesday, June 15, 2011, 1:40 AM



 
 
 
 




 

Teman2,
 
   
Di dalam SCAL, ada perhitungan formation resistivity factor a, m dan n yang 
digunakan dalam petrophysics nantinya. 
Di dalam pengukurannya, ada yang diukur dalam lingkungan ambient, ada yang di 
lingkungan overburden (formation pressure). 
Apakah biasanya teman2 melakukan kedua-duanya dalam analisa atau hanya 
melakukan yang overburden? 
Biasanya berapa banyak selisihnya, apakah sensitif?  
   
Terimakasih banyak, 
   
Parvita
 H. Siregar 
Chief Geologist
 
Salamander Energy Indonesia 
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