dc.contributorhttps://orcid.org/0000-0002-8302-2736
dc.contributorhttps://orcid.org/0000-0001-5272-4447
dc.contributorhttps://orcid.org/0000-0002-4479-5795
dc.contributorhttps://scholar.google.com/citations?hl=es&user=m5VhA7cAAAAJ
dc.contributorhttps://scholar.google.com/citations?hl=es&user=OuVxcUgAAAAJ
dc.contributorhttps://scholar.google.com/citations?hl=es&user=vL7TGssAAAAJ
dc.contributorhttps://scienti.minciencias.gov.co/cvlac/visualizador/generarCurriculoCv.do?cod_rh=0000650579
dc.contributorhttps://scienti.minciencias.gov.co/gruplac/jsp/visualiza/visualizagr.jsp?nro=00000000007553
dc.creatorJaramillo Barrios, Camilo Ignacio
dc.creatorOrtiz Rico, Andrés Felipe
dc.creatorAraujo Carrillo, Gustavo Alfonso
dc.creatorVarón Ramírez, Viviana Marcela
dc.date.accessioned2020-02-26T18:00:39Z
dc.date.accessioned2022-09-28T13:35:06Z
dc.date.available2020-02-26T18:00:39Z
dc.date.available2022-09-28T13:35:06Z
dc.date.created2020-02-26T18:00:39Z
dc.date.issued2020-02-26
dc.identifierJaramillo-Barrios, C. I., Ortiz-Rico, A. F., Carrillo, G. A. A., & Varón-Ramírez, V. M. (2019). Establishment of homogeneous zones in a soil of alluvial origin. Ciência E Agrotecnologia, 43 doi:10.1590/1413-7054201943026318
dc.identifierhttp://hdl.handle.net/11634/21882
dc.identifierhttps://doi.org/10.1590/1413-7054201943026318
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3641119
dc.description.abstractSoils have the ability to maintain plant growth and biological activity due to their physical and chemical properties. The aim of this study was to observe the spatial distribution of some chemical properties of the soil, such as pH, organic matter (OM), electrical conductivity (EC), effective cation exchange capacity (ECEC), sulfur (S) and aluminum (Al) content and to establish zones with homogeneous chemical characteristics using the MULTISPATI-PCA technique and the fuzzy c-means algorithm. The study area was located in the Tundama and Sugamuxi Valleys (Boyacá, Colombia) with an area of 8,017 ha. Chemical properties such as pH, OM, EC, S, Al, and ECEC were indicators of the chemical degradation of these soils. Four homogeneous zones were identified. The first zone represents areas with acidity and excessive sulfur, with a pH of 4.54, 15.88% OM, 3.19 dS m-1 EC, 2.47 meq 100 g-1 Al and 365.59 meq 100 g-1 S. In contrast, the second zone represents areas with a high self-neutralizing capacity, with a pH of 5.98, 4.22% OM, 0.75 dS m-1 EC, 0.20 meq 100 g-1 Al and 44.64 meq 100 g-1 S. Zone three showed a high similarity with the first two, except for its EC and S contents. Finally, zone four showed similarity with the first, except in OM, EC and S contents. These data show that S and EC influenced the homogeneous zones because the soils in this area are called acid sulfate soils
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dc.rightshttp://creativecommons.org/licenses/by-nc-sa/2.5/co/
dc.rightsAtribución-NoComercial-CompartirIgual 2.5 Colombia
dc.titleEstablishment of homogeneous zones in a soil of alluvial origin
dc.typeApropiación Social y Circulación del Conocimiento: Alianzas con centros dedicados a la apropiación social del conocimiento


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