Rock magnetic investigations of surface and sub-surface soil samples from five lake catchments in tropical southern India

K. Sandeep, A. K. Warrier, B. G. Harshavardhana, R. Shankar

Research output: Contribution to journalArticle

13 Citations (Scopus)

Abstract

Iron oxide minerals in soils provide valuable insights into pedogenic processes. A wealth of such information has been obtained by rock magnetic investigations on temperate soils but similar studies on tropical soils are rare. Here, we report rock magnetic data on pristine soil profiles and surficial soils from five catchments in the tropical southern India and throw light on the pedogenic processes. We ruled out contributions from greigite, bacterial magnetite and anthropogenic sources; hence, the magnetic signal is mainly from the catchment, principally pedogenic and, thus, has a climatic signature embedded in it. The Pookot profile from a high rainfall (~4000 mm/year) region does not exhibit any magnetic enhancement at the surface. In fact, there is hardly any difference between surface and sub-surface samples, which reflects on its deeply weathered nature as a result of the high rainfall. The Shantisagara profile exhibits lessivage of magnetic minerals, resulting in a thick magnetically enhanced zone. It shows the highest χ lf values among the five profiles studied. The Thimmannanayakanakere (TK) and Ayyanakere (AK) soil profiles do not exhibit any magnetic enhancement of top-soil. In fact, χ lf values increase towards the profile-bottom, suggesting top-soil erosion, besides contribution of magnetic minerals from parent rocks. In the TK profile, there is a clear distinction between surface and sub-surface samples, the former being magnetically coarser grained. The Kurburukere profile exhibits moderate to strong χ lf values and a mild magnetic enhancement at the surface.The data would be useful for establishing soil-sediment linkages for paleoclimatic studies of lake sediments.

Original languageEnglish
Pages (from-to)1-18
Number of pages18
JournalInternational Journal of Environmental Research
Volume6
Issue number1
Publication statusPublished - 01-01-2012

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soil surface
catchment
lake
rock
magnetic mineral
topsoil
soil profile
soil
greigite
rainfall
tropical soil
anthropogenic source
iron oxide
soil erosion
lacustrine deposit
magnetite
mineral
sediment

All Science Journal Classification (ASJC) codes

  • Environmental Science(all)

Cite this

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abstract = "Iron oxide minerals in soils provide valuable insights into pedogenic processes. A wealth of such information has been obtained by rock magnetic investigations on temperate soils but similar studies on tropical soils are rare. Here, we report rock magnetic data on pristine soil profiles and surficial soils from five catchments in the tropical southern India and throw light on the pedogenic processes. We ruled out contributions from greigite, bacterial magnetite and anthropogenic sources; hence, the magnetic signal is mainly from the catchment, principally pedogenic and, thus, has a climatic signature embedded in it. The Pookot profile from a high rainfall (~4000 mm/year) region does not exhibit any magnetic enhancement at the surface. In fact, there is hardly any difference between surface and sub-surface samples, which reflects on its deeply weathered nature as a result of the high rainfall. The Shantisagara profile exhibits lessivage of magnetic minerals, resulting in a thick magnetically enhanced zone. It shows the highest χ lf values among the five profiles studied. The Thimmannanayakanakere (TK) and Ayyanakere (AK) soil profiles do not exhibit any magnetic enhancement of top-soil. In fact, χ lf values increase towards the profile-bottom, suggesting top-soil erosion, besides contribution of magnetic minerals from parent rocks. In the TK profile, there is a clear distinction between surface and sub-surface samples, the former being magnetically coarser grained. The Kurburukere profile exhibits moderate to strong χ lf values and a mild magnetic enhancement at the surface.The data would be useful for establishing soil-sediment linkages for paleoclimatic studies of lake sediments.",
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Rock magnetic investigations of surface and sub-surface soil samples from five lake catchments in tropical southern India. / Sandeep, K.; Warrier, A. K.; Harshavardhana, B. G.; Shankar, R.

In: International Journal of Environmental Research, Vol. 6, No. 1, 01.01.2012, p. 1-18.

Research output: Contribution to journalArticle

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