Bioquímica de suelos derivados de cenizas volcánicas. VII. Determinación de deshidrogenasas.
Author | dc.contributor.author | Aguilera S., S. María | |
Author | dc.contributor.author | Borie B., Gilda | es_CL |
Author | dc.contributor.author | Rokov C., Pamela | es_CL |
Author | dc.contributor.author | Peirano V., Pedro | es_CL |
Admission date | dc.date.accessioned | 2010-09-07T16:29:07Z | |
Available date | dc.date.available | 2010-09-07T16:29:07Z | |
Publication date | dc.date.issued | 1988-04 | |
Cita de ítem | dc.identifier.citation | Agricultura Técnica (Chile) 48(2): 147-151 | en_US |
Identifier | dc.identifier.issn | 0365-2807 | |
Identifier | dc.identifier.uri | https://repositorio.uchile.cl/handle/2250/121034 | |
Abstract | dc.description.abstract | Dehydrogenase and respiratory activities were studies in six soils, five of volcanic origin and the other alluvial, as a reference. Dehydrogenases activity was measured by the reduction of 2, 3, 5- Tryphenyl Tetrazolium Chloride (TTC)to Triphenylformazan (TFF). TFF being deep red, facilitates its quantification by spectrophotometry. The Osorno soil exhibited the highest contents of dehydrogenases, followed by Corte Alto, Frutillar and Arrayán, all of them being of volcanic origin and having high content of organic matter. Puerto Octay showed values similar to Olivos, which is alluvial and of a low content of organic matter. The effect of humidity levels on dehydrogenases content varied according to soil characteristics. TFF adsorption by these soils turned out to be very high. | en_US |
Lenguage | dc.language.iso | es | en_US |
Publisher | dc.publisher | Instituto de Investigaciones Agropecuarias | en_US |
Keywords | dc.subject | Cenizas volcánicas | en_US |
Título | dc.title | Bioquímica de suelos derivados de cenizas volcánicas. VII. Determinación de deshidrogenasas. | en_US |
Document type | dc.type | Artículo de revista |
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