Environmental magnetism: Difference between revisions

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'''Environmental magnetism''' is the study of [[magnetism]] as it relates to the effects of [[climate]], [[sediment transport]], [[pollution]] and other environmental influences on magnetic minerals. It makes use of techniques from [[rock magnetism]] and [[magnetic mineralogy]]. There are two advantages to using magnetic measurements to study these subjects: (1) magnetic minerals are almost ubiquitous and (2) magnetic measurements are quick and non-invasive.
'''Environmental magnetism''' is the study of [[magnetism]] as it relates to the effects of [[climate]], [[sediment transport]], [[pollution]] and other environmental influences on magnetic minerals. It makes use of techniques from [[rock magnetism]] and [[magnetic mineralogy]]. The magnetic properties of minerals are used as proxies for environmental change in applications such as [[paleoclimate]], [[paleoceanography]], studies of the [[provenance]] of sediments, [[pollution]] and [[archeology]].<ref>{{harvnb|Dekkers|1997}}</ref> The main advantages of using magnetic measurements are that magnetic minerals are almost ubiquitous and magnetic measurements are quick and non-invasive.


== History ==
== History ==
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== References ==
== References ==
*{{cite journal
*{{cite journal
|last1 = Oldfield
|last1=Dekkers
|first1 = F.
|first1=M. J.
|title=Environmental magnetism: an introduction
|last2 = Dearing
|journal = Geologie en Mijnbouw
|first2 = J.A.
|volume=76
|last3 = Thompson
|number=1&mdash;2
|first3 = R.
|pages=163&mdash;182
|last4 = Garret-Jones
|doi=10.1023/A:1003122305503
|first4 = S.E.
|ref=harvnb
|title = Some magnetic properties of lake sediments and their possible links with erosion rates.
|journal = Polskie Archive. Hydrobiologia
|volume = 25
|pages = 321-331
|year = 1978
}}
}}
*{{cite book
*{{cite book
Line 41: Line 37:
|year = 1997
|year = 1997
|isbn = 0-521-32514-5
|isbn = 0-521-32514-5
|ref=harvnb
}}
}}
*{{cite book
*{{cite book
Line 51: Line 48:
|year = 2003
|year = 2003
|isbn = 0-12-243851-5
|isbn = 0-12-243851-5
|ref=harvnb
}}
*{{cite book
|last1 = Thompson
|first1 = R.
|last2 = Oldfield
|first2 = F.
|title = Environmental Magnetism
|publisher = [[Allen and Unwin]]
|year = 1986
|isbn = 9780045380039
}}
}}
*{{cite book
*{{cite book
Line 71: Line 59:
|year = 1999
|year = 1999
|isbn = 0521624177
|isbn = 0521624177
|ref=harvnb
}}
}}
*{{cite journal
*{{cite journal
Line 81: Line 70:
|year = 1988
|year = 1988
|doi = 10.1111/j.1365-246X.1988.tb03429.x
|doi = 10.1111/j.1365-246X.1988.tb03429.x
}}
*{{cite journal
|last1 = Oldfield
|first1 = F.
|last2 = Dearing
|first2 = J.A.
|last3 = Thompson
|first3 = R.
|last4 = Garret-Jones
|first4 = S.E.
|title = Some magnetic properties of lake sediments and their possible links with erosion rates.
|journal = Polskie Archive. Hydrobiologia
|volume = 25
|pages = 321-331
|year = 1978
|ref=harvnb
}}
*{{cite book
|last1 = Thompson
|first1 = R.
|last2 = Oldfield
|first2 = F.
|title = Environmental Magnetism
|publisher = [[Allen and Unwin]]
|year = 1986
|isbn = 9780045380039
|ref=harvnb
}}
}}
*{{cite journal
*{{cite journal

Revision as of 00:33, 2 September 2011

Environmental magnetism is the study of magnetism as it relates to the effects of climate, sediment transport, pollution and other environmental influences on magnetic minerals. It makes use of techniques from rock magnetism and magnetic mineralogy. The magnetic properties of minerals are used as proxies for environmental change in applications such as paleoclimate, paleoceanography, studies of the provenance of sediments, pollution and archeology.[1] The main advantages of using magnetic measurements are that magnetic minerals are almost ubiquitous and magnetic measurements are quick and non-invasive.

History

Environmental magnetism was first identified as a distinct field in 1978[2] and was introduced to a wider audience by the book Environmental Magnetism in 1986.[3] Since then it has grown rapidly, finding application in and making major contributions to a range of diverse fields, especially paleoclimate, sedimentology, paleoceanography, and studies of particulate pollution.[4]. [5].

Fundamentals

Environmental magnetism is built on two parts of rock magnetism: magnetic mineralogy, which looks at how basic magnetic properties depend on composition; and magnetic hysteresis, which can provide details on particle size and other physical properties that also affect the hysteresis. Several parameters have been developed to represent certain features of the hysteresis.[6] [7]

See also

Notes

  1. ^ Dekkers 1997
  2. ^ Oldfield & et al. 1978
  3. ^ Thompson & Oldfield 1986
  4. ^ Maher & Thompson 1999
  5. ^ Evans & Heller 2003
  6. ^ Dunlop & Özdemir 1997
  7. ^ Maher 1998

References

  • Dekkers, M. J. "Environmental magnetism: an introduction". Geologie en Mijnbouw. 76 (1–2): 163–182. doi:10.1023/A:1003122305503.
  • Dunlop, David J.; Özdemir, Özden (1997). Rock magnetism: Fundamentals and Frontiers. Cambridge Univ. Press. ISBN 0-521-32514-5.
  • Evans, Michael E.; Heller, Friedrich (2003). Environmental Magnetism: Principles and Applications of Enviromagnetics. Academic Press. ISBN 0-12-243851-5.
  • Maher, B.A.; Thompson, R. (1999). Quaternary Environments, Climates and Magnetism. Cambridge University Press. ISBN 0521624177.
  • Maher, B.A. (1988). "Magnetic properties of some synthetic sub-micron magnetites". Geophys. J. Roy. Astr. Soc. 94: 83–96. doi:10.1111/j.1365-246X.1988.tb03429.x.
  • Oldfield, F.; Dearing, J.A.; Thompson, R.; Garret-Jones, S.E. (1978). "Some magnetic properties of lake sediments and their possible links with erosion rates". Polskie Archive. Hydrobiologia. 25: 321–331.
  • Thompson, R.; Oldfield, F. (1986). Environmental Magnetism. Allen and Unwin. ISBN 9780045380039.
  • Verosub, Kenneth L.; Roberts, Andrew P. (1995). "Environmental magnetism: Past, present and future". J. Geophys. Res. 100: 2175–2192. doi:10.1029/94JB02713.