{"id":114835,"date":"2013-08-11T00:00:00","date_gmt":"2013-08-11T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/modelizacion-de-propiedades-fa%c2%adsicas-del-suelo-a-escala-regional-casos-de-estudio-en-el-sureste-iberico\/"},"modified":"2013-08-11T00:00:00","modified_gmt":"2013-08-11T00:00:00","slug":"modelizacion-de-propiedades-fa%c2%adsicas-del-suelo-a-escala-regional-casos-de-estudio-en-el-sureste-iberico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/edafologia\/modelizacion-de-propiedades-fa%c2%adsicas-del-suelo-a-escala-regional-casos-de-estudio-en-el-sureste-iberico\/","title":{"rendered":"Modelizaci\u00f3n de propiedades f\u00edsicas del suelo a escala regional. casos de estudio en el sureste ib\u00e9rico."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Pedro Perez Cutillas <\/strong><\/h2>\n<p>Resumen memoria de tesis modelizaci\u00f3n de propiedades f\u00edsicas del suelo a escala regional. Casos de estudio en el sureste ib\u00e9rico  pedro p\u00e9rez cutillas licenciado en geograf\u00eda e historia memoria presentada para optar al grado de doctor murcia, 2013  objetivos generales  la finalidad de esta memoria de tesis es combinar la aplicabilidad de herramientas sig y teledetecci\u00f3n con la modelizaci\u00f3n estad\u00edstica de variables ambientales a escala regional,  aportando de manera concreta resultados y conclusiones que ayuden a mejorar las estimaciones de las propiedades del suelo. La textura, como principal propiedad f\u00edsica del suelo, desempe\u00f1a una funci\u00f3n esencial en la estructura de esta memoria, present\u00e1ndose como nexo de uni\u00f3n del resto de an\u00e1lisis expuestos en este trabajo. Sin pretender entrar en complejos an\u00e1lisis de las propiedades qu\u00edmicas del suelo se han obtenido estimaciones de carbono y materia org\u00e1nica del suelo, necesarios para el estudio de la din\u00e1mica del agua en el suelo. Su interacci\u00f3n con la textura nos permitir\u00e1 abordar la estimaci\u00f3n regional del contenido del contenido de agua a capacidad de campo y en el punto de marchitamiento, determinando cu\u00e1les son las variables ambientales que inciden de manera m\u00e1s importante en esas propiedades f\u00edsicas del suelo. En \u00faltimo lugar, se mostrar\u00e1 c\u00f3mo la disponibilidad de mapas regionales de la textura del suelo elaborados en este trabajo influyen en nuestra estimaci\u00f3n de los procesos de degradaci\u00f3n del suelo, evaluado mediante el an\u00e1lisis de la erosionabilidad y su efecto en modelos de erosi\u00f3n.      a continuaci\u00f3n se exponen los cap\u00edtulos realizados:  cap\u00edtulo 1. Se han determinado cu\u00e1les son las variables ambientales que m\u00e1s influyen en la textura. Y se han analizado los efectos que se producen en la modificaci\u00f3n de la resoluci\u00f3n espacial en los valores de las variables ambientales que forman parte de los modelos de estimaci\u00f3n de la textura del suelo.  Cap\u00edtulo 2. Se ha evaluado y comparado dos m\u00e9todos de estimaci\u00f3n del potencial de succi\u00f3n (pf) a escala regional: el primer m\u00e9todo es una estimaci\u00f3n directa del contenido de humedad del suelo mediante la modelizaci\u00f3n con valores emp\u00edricos de las propiedades h\u00eddricas. El segundo procedimiento de estimaci\u00f3n se basa en un m\u00e9todo indirecto mediante el uso de los datos texturales (obtenidos en el cap\u00edtulo 1) y de materia org\u00e1nica (om) en funciones de pedotransferencia ya publicadas. Cap\u00edtulo 3. Se han comparado dos m\u00e9todos de estimaci\u00f3n de diversos \u00edndices de erosionabilidad relativos al factor k de la usle. El primer m\u00e9todo utiliza las propiedades f\u00edsico &#8211; qu\u00edmicas del suelo (texturas y om) promedio de cada tipo de suelo y realiza una translaci\u00f3n de las mismas a la cartograf\u00eda de suelos existente. Mediante el segundo m\u00e9todo se aplican los resultados de la modelizaci\u00f3n de texturas y om obtenidas en los cap\u00edtulos 1 y 2, respectivamente.           dissertation abstract modelling of soil physical properties at regional scale. Case studies in the iberian southeast  pedro p\u00e9rez cutillas degree in geography and history dissertation presented for ph. Degree murcia, 2013  the aim of this thesis is to combine the applicability of gis and remote sensing tools with statistical modeling of regional scale of environmental variables to provide results and conclusions and improve estimates of soil properties. Soil texture plays a key role in the structure of this report, being connecting link of other analyzes presented in this paper. Organic carbon and soil organic matter estimates were obtained for the study of the dynamics of soil water. Interaction with the texture allows regional estimates of water content at field capacity and wilting point, showing the environmental variables most affecting soil physical properties. Finally, we prove how the availability of regional maps of soil texture developed in this work influence our estimation of soil degradation processes, assessed by analyzing the effect on erodibility and erosion models.  below the chapters performed:  chapter 1. Dave determined what environmental variables that influence texture. And we have analyzed the effects of changing spatial resolution on the values of the environmental variables on the models for estimating soil texture. Chapter 2. We evaluated and compared two methods of estimating matric potential (pf) at regional scale. The first method is to estimate the soil moisture through modeling with empirical values water properties. Second estimation method is by using textural data (chapter 1) and organic matter (om) using pedotransfer functions (ptfs). Chapter 3. We compared two different methods of estimating erodibility indices relating to k factor (usle). First method uses the physical &#8211; chemical properties of the soil (texture and om) average of each soil type by translational soil mapping. Second applies the results of modeling of textures and om obtained in chapters 1 and 2, respectively.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Modelizaci\u00f3n de propiedades f\u00edsicas del suelo a escala regional. casos de estudio en el sureste ib\u00e9rico.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Modelizaci\u00f3n de propiedades f\u00edsicas del suelo a escala regional. casos de estudio en el sureste ib\u00e9rico. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Pedro Perez Cutillas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Murcia<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 08\/11\/2013<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Gonzalo Gonz\u00e1lez Barber\u00e1<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Francisco Lopez bermudez <\/li>\n<li>Mar\u00eda Martinez-mena garcia (vocal)<\/li>\n<li>roberto Tom\u00e1s jover (vocal)<\/li>\n<li>Jos\u00e9 dami\u00e1n Ruiz sinoga (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Pedro Perez Cutillas Resumen memoria de tesis modelizaci\u00f3n de propiedades f\u00edsicas del suelo a escala regional. Casos [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[2498,5741,8235,13542],"tags":[24919,173665,209291,25093,227462,190604],"class_list":["post-114835","post","type-post","status-publish","format-standard","hentry","category-edafologia","category-geografia-fisica","category-murcia","category-sistemas-de-informacion-geografica","tag-francisco-lopez-bermudez","tag-gonzalo-gonzalez-barbera","tag-jose-damian-ruiz-sinoga","tag-maria-Martinez-mena-garcia","tag-pedro-perez-cutillas","tag-roberto-tomas-jover"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/114835","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=114835"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/114835\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=114835"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=114835"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=114835"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}