Preamble
Rocks and sediments
inevitably contain mixtures of magnetic minerals, grain sizes, and
weathering states. Most rock magnetic interpretation techniques rely on
a set of value parameters, such as susceptibility and
isothermal/anhysteretic remanent magnetisation (ARM or IRM). These
parameters are usually interpreted in terms of mineralogy and domain
state of the magnetic particles. In some cases, such interpretation of
natural samples may be misleading or inconclusive.
A less constrained approach to magnetic mineralogy models is based on
the analysis of magnetisation curves, which are decomposed into a set
of elementary contributions. Each contribution is called a magnetic
component, and characterises a specific set of magnetic grains with a
unimodal distribution of physical and chemical properties. Magnetic
components are related to specific biogeochemical signatures rather
than representing traditional categories, such as single domain
magnetite. This unconventional approach can be regarded as a kind of
principal component analysis (PCA) that gives a direct link to the
interpretation of natural processes on a multidisciplinary level. Since
magnetic components rarely occur alone in natural samples, unmixing
techniques and rock magnetic models are interdependent.
Valuable information
for rock magnetic and environmental studies can be obtained directly
from the coercivity distribution of the sample, which provides a
richness of details hidden in the measurement curve.
What
is MAG-MIX?
The software
package MAG-MIX provides computer programmes for the analysis of
isothermal magnetisation curves* and coercivity
distributions and was developed by Ramon Egli. This
first release includes the programmes CODICA and GECA. It
consists of two packages: CODICA (COercivity
DIstribution CAlculator)
and GECA (GEneralised Coercivity Analyser).
*The
term magnetisation curve has here and in the following the meaning of
an acquisition curve, alternating field demagnetisation curve or
backfield curve (latter also called direct current demagnetisation).
What
does CODICA do?
CODICA is
a programme that calculates the coercivity distribution of a
magnetisation curve and estimates the measurement errors. CODICA
eliminates efficiently measurement noise from
acquisition or demagnetisation curves of remanent magnetisation (based
on rescaling procedures)
and calculates then the derivative (also called coercivity
distribution or coercivity spectrum).
What
does Geca do?
GECA is a
programme for modelling a coercivity distribution as a linear
combination
of special model functions, that are supposed to represent the
coercivity distribution of specific groups of magnetic particles,
called components (= unmixing). A Pearson's X
2
goodness of fit test evaluates the number of functions required for the
best-fit and an error estimation allows to calculate the confidence
limit for each model parameter.
Requirements
Both
programmes are written in Mathematica,
a programming language similar to other traditional computer languages
such as C, Pascal or FORTRAN. The usage of CODICA implies that Mathematica is installed on
your computer. MAG-MIX has been developed for Mathematica
5.0 under Windows, but with small code modifications it is also
compatible with Mathematica for
Linux/Unix. At least 128 MB RAM
and a 1 GHz CPU are recommended.
Installation
1.
Install Mathematica on your computer.
2. Download the
zip-file from below, store it in a local directory and unpack it.
3. Install
CODICA. To install CODICA 5.0 copy the source code file MAG_MIX_1/CODICA/Install/Codica.m
into the following directory:
C:/.../WolframResearch/Mathematica/5.0/AddOns/StandardPackages/Utilities
whereby C:/.../ depends on the
installation of Mathematica on your computer.
4. To install GECA, copy the source code file MAG_MIX_1/GECA/Install/Geca.m
and the file MAG_MIX_1/GECA/Install/components.txt
into the
following directory:
C:/.../Wolfram
Research/Mathematica/5.0/AddOns/StandardPackages/Utilities
whereby C:/.../ depends
on the installation of Mathematica on your computer.
Download
Both
releases can be
downloaded following the links below.
MAG-MIX
Release 1 (2005), Mathematica v.5.0 for Windows must be
installed in your computer.
The zip file
contains: installation instructions for CODICA 5.0 and
GECA
2.1, the source code (files Codica.m,
Geca.m),
the reference manual (pdf-format) and examples (including data).
Manual
only
Here you can
download the reference manual, including theoretical aspects.
Notice
Your feedback is
important to improve the MAG-MIX. If you encounter problems in
using the programmes, or if you have suggestions, please do not hesitate to
contact the author by
e-mail: eglix007@umn.edu.
References
Egli, R.,
Analysis of the field
dependence of remanent magnetization curves, Journal
of Geophysical
Research, 108 (B2),
2081, doi 10.1029/2002JB002023, 2003.
Egli,
R., Characterization of individual rock
magnetic components by analysis of remanence curves, 2. fundamental
properties of coercivity distributions, Physics and Chemistry of the Earth,
29, 851-867, 2004.
Heslop,
D., Dekkers, M.J., Kruiver, P.P. and I. H.
M. van Oorschot, Analysis of isothermal remanent magnetization
acquisition curves using the expectation-maximization algorithm, Geophysical Journal International,148, 58-64, 2002.
Kruiver
P.P., Dekkers M.J. and D. Heslop, Quantification of
magnetic coercivity components by the analysis of acquisition curves of
isothermal remanent magnetisation, Earth and Planetary Science Letters, 189,
269-276,
2001.
Spassov,
S., Egli, R., Heller, F., Nourgaliev, D.K. and J. Hannam, Magnetic
quantification of urban pollution sources in atmospheric particulate
matter, Geophysical Journal
International, 159,
555-564, 2004.