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        <Text language="fre">&lt;p&gt;&lt;b&gt;Cet ouvrage en impression à la demande sera envoyé sous 3 semaines environ (France métropolitaine) et dans un colis séparé en cas de commande avec un autre livre papier.&lt;/b&gt;&lt;/p&gt;&lt;p&gt;Le référentiel pédologique est une typologie de´taille´e des sols de notre territoire, de l'Europe, de l'Afrique et des autres continents. Entièrement remanié, ce nouveau millésime du &lt;em&gt;Référentiel pédologique &lt;/em&gt;s'est enrichi de trois nouveaux chapitres traitant de solums des zones intertropicales et de leurs horizons de référence spécifiques, ainsi que de deux outils inédits&amp;nbsp;: une clé d'accès rapide aux différents chapitres et une annexe des correspondances possibles entre les références du &lt;em&gt;Référentiel pédologique &lt;/em&gt;et les catégories de la &lt;em&gt;World reference Base for soil resources&lt;/em&gt;.&lt;br&gt;À l'épreuve du terrain depuis plus de quinze ans, le référentiel pédologique est désormais incontournable. Conçu pour être accessible aux non spécialistes qui maîtrisent le vocabulaire de base de la pédologie, il est indispensable à tous ceux qui doivent prendre en compte la diversité des sols.&lt;/p&gt;</Text>
        <Text language="eng">&lt;p&gt;&lt;b&gt;This Print On Demand book will be sent within 3 weeks (metropolitan France) and in a separate package if you order another paperback book.&lt;/b&gt;&lt;/p&gt;&lt;p&gt;The Référentiel pédologique is a detailed typology of soils in France, Europe, Africa and other continents. The new edition, which has been entirely reworked, contains three new chapters covering solums in intertropical zones and their specific reference horizons, and two new tools: a rapid access key to the different chapters and an annexe of the possible correspondences between the references in the &lt;em&gt;Référentiel pédologique &lt;/em&gt;and the categories in the &lt;em&gt;World Reference Base for Soil Resources&lt;/em&gt;. The &lt;em&gt;Référentiel pédologique &lt;/em&gt;has been tried and tested in the field for some fifteen years now, and has become indispensable. It was designed to be accessible to non-specialists with some knowledge of the basic vocabulary of soil science, and is indispensable to anyone wanting to take account of the diversity of soil types.&lt;/p&gt;</Text>
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        <Text>Entièrement remanié et enrichi, ce millésime 2008 du Référentiel pédologique permet de désigner les sols et de les rattacher à un système de références. Outil irremplaçable pour effectuer des corrélations et transmettre une information riche.</Text>
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        <Text>&lt;p&gt;Pr&amp;eacute;face&lt;br /&gt;&lt;br /&gt;Avertissement&lt;br /&gt;&lt;br /&gt;Pourquoi un r&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique ?&lt;br /&gt;&lt;br /&gt;Auteurs et collaborateurs&lt;br /&gt;&lt;br /&gt;Liste des horizons de r&amp;eacute;f&amp;eacute;rence du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt;&lt;br /&gt;D&amp;eacute;finition des horizons de r&amp;eacute;f&amp;eacute;rence&lt;br /&gt;Liste et d&amp;eacute;finitions des qualificatifs&lt;br /&gt;Qualificatifs class&amp;eacute;s par th&amp;egrave;mes&lt;br /&gt;Vocabulaire pour les pal&amp;eacute;osolums&lt;br /&gt;Tol&amp;eacute;rances pour les crit&amp;egrave;res num&amp;eacute;riques &amp;ndash; R&amp;egrave;gles d&amp;#39;&amp;eacute;critures&lt;br /&gt;Cl&amp;eacute; pour trouver rapidement une r&amp;eacute;f&amp;eacute;rence de rattachement&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Pr&amp;eacute;sentation des grands ensembles de r&amp;eacute;f&amp;eacute;rences (GER)&lt;br /&gt;&lt;/strong&gt;Alocrisols&lt;br /&gt;Andosols&lt;br /&gt;Anthroposols&lt;br /&gt;Ar&amp;eacute;nosols&lt;br /&gt;Brunisols&lt;br /&gt;Solums dont le complexe adsorbant est domin&amp;eacute; par le calcium (et/ou le magn&amp;eacute;sium)&lt;br /&gt;Chernosols&lt;br /&gt;Colluviosols&lt;br /&gt;Cryosols&lt;br /&gt;Ferrallitisols et oxydisols&lt;br /&gt;Ferruginosols&lt;br /&gt;Fersialsols&lt;br /&gt;Fluviosols&lt;br /&gt;Grisols&lt;br /&gt;Gypsosols&lt;br /&gt;Histosols&lt;br /&gt;Leptismectisols&lt;br /&gt;Lithosols&lt;br /&gt;Luvisols&lt;br /&gt;Nitosols&lt;br /&gt;Organosols&lt;br /&gt;P&amp;eacute;losols&lt;br /&gt;Peyrosols&lt;br /&gt;Ph&amp;aelig;osols&lt;br /&gt;Planosols&lt;br /&gt;Podzosols&lt;br /&gt;Rankosols&lt;br /&gt;R&amp;eacute;ductisols et r&amp;eacute;doxisols&lt;br /&gt;R&amp;eacute;gosols&lt;br /&gt;Salisols et sodisols&lt;br /&gt;Thalassosols&lt;br /&gt;Thiosols et sulfatosols&lt;br /&gt;Veracrisols&lt;br /&gt;Vertisols&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Annexes&lt;/strong&gt;&lt;br /&gt;1 &amp;ndash; Typologie des formes&amp;nbsp; d&amp;rsquo;humus foresti&amp;egrave;res&lt;br /&gt;2 &amp;ndash; El&amp;eacute;ments pour l&amp;rsquo;&amp;eacute;tablissement d&amp;rsquo;un r&amp;eacute;f&amp;eacute;rentiel pour les solums hydromorphes&lt;br /&gt;3 &amp;ndash; M&amp;eacute;thodes d&amp;rsquo;analyses pr&amp;eacute;conis&amp;eacute;es&lt;br /&gt;4 &amp;ndash; Termes relatifs aux teneurs en carbone organique&lt;br /&gt;5 &amp;ndash; Correspondances possibles entre r&amp;eacute;f&amp;eacute;rences du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt; et RSG de la &lt;em&gt;World Reference Base&lt;/em&gt; (2006)&lt;br /&gt;6 &amp;ndash; Correspondance des horizons entre syst&amp;egrave;mes CPCS et &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt;&lt;br /&gt;7 &amp;ndash; Correspondances possibles entre cat&amp;eacute;gories de la classification CPCS et &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt;&lt;br /&gt;8 &amp;ndash; Possibilit&amp;eacute; de regroupement des GER en quatorze cat&amp;eacute;gories&lt;br /&gt;9 &amp;ndash; Lexique&lt;br /&gt;&lt;br /&gt;Liste des 110 r&amp;eacute;f&amp;eacute;rences du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008 &lt;/em&gt;(par chapitres)&lt;br /&gt;Liste des 110 r&amp;eacute;f&amp;eacute;rences du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008 &lt;/em&gt;(par ordre alphab&amp;eacute;tique)&lt;br /&gt;&amp;nbsp;&lt;/p&gt;</Text>
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        <Text>&lt;p&gt;Pr&amp;eacute;face&lt;br /&gt;&lt;br /&gt;Avertissement&lt;br /&gt;&lt;br /&gt;Pourquoi un r&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique ?&lt;br /&gt;&lt;br /&gt;Auteurs et collaborateurs&lt;br /&gt;&lt;br /&gt;Liste des horizons de r&amp;eacute;f&amp;eacute;rence du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt;&lt;br /&gt;D&amp;eacute;finition des horizons de r&amp;eacute;f&amp;eacute;rence&lt;br /&gt;Liste et d&amp;eacute;finitions des qualificatifs&lt;br /&gt;Qualificatifs class&amp;eacute;s par th&amp;egrave;mes&lt;br /&gt;Vocabulaire pour les pal&amp;eacute;osolums&lt;br /&gt;Tol&amp;eacute;rances pour les crit&amp;egrave;res num&amp;eacute;riques &amp;ndash; R&amp;egrave;gles d&amp;#39;&amp;eacute;critures&lt;br /&gt;Cl&amp;eacute; pour trouver rapidement une r&amp;eacute;f&amp;eacute;rence de rattachement&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Pr&amp;eacute;sentation des grands ensembles de r&amp;eacute;f&amp;eacute;rences (GER)&lt;br /&gt;&lt;/strong&gt;Alocrisols&lt;br /&gt;Andosols&lt;br /&gt;Anthroposols&lt;br /&gt;Ar&amp;eacute;nosols&lt;br /&gt;Brunisols&lt;br /&gt;Solums dont le complexe adsorbant est domin&amp;eacute; par le calcium (et/ou le magn&amp;eacute;sium)&lt;br /&gt;Chernosols&lt;br /&gt;Colluviosols&lt;br /&gt;Cryosols&lt;br /&gt;Ferrallitisols et oxydisols&lt;br /&gt;Ferruginosols&lt;br /&gt;Fersialsols&lt;br /&gt;Fluviosols&lt;br /&gt;Grisols&lt;br /&gt;Gypsosols&lt;br /&gt;Histosols&lt;br /&gt;Leptismectisols&lt;br /&gt;Lithosols&lt;br /&gt;Luvisols&lt;br /&gt;Nitosols&lt;br /&gt;Organosols&lt;br /&gt;P&amp;eacute;losols&lt;br /&gt;Peyrosols&lt;br /&gt;Ph&amp;aelig;osols&lt;br /&gt;Planosols&lt;br /&gt;Podzosols&lt;br /&gt;Rankosols&lt;br /&gt;R&amp;eacute;ductisols et r&amp;eacute;doxisols&lt;br /&gt;R&amp;eacute;gosols&lt;br /&gt;Salisols et sodisols&lt;br /&gt;Thalassosols&lt;br /&gt;Thiosols et sulfatosols&lt;br /&gt;Veracrisols&lt;br /&gt;Vertisols&lt;br /&gt;&lt;br /&gt;&lt;strong&gt;Annexes&lt;/strong&gt;&lt;br /&gt;1 &amp;ndash; Typologie des formes&amp;nbsp; d&amp;rsquo;humus foresti&amp;egrave;res&lt;br /&gt;2 &amp;ndash; El&amp;eacute;ments pour l&amp;rsquo;&amp;eacute;tablissement d&amp;rsquo;un r&amp;eacute;f&amp;eacute;rentiel pour les solums hydromorphes&lt;br /&gt;3 &amp;ndash; M&amp;eacute;thodes d&amp;rsquo;analyses pr&amp;eacute;conis&amp;eacute;es&lt;br /&gt;4 &amp;ndash; Termes relatifs aux teneurs en carbone organique&lt;br /&gt;5 &amp;ndash; Correspondances possibles entre r&amp;eacute;f&amp;eacute;rences du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt; et RSG de la &lt;em&gt;World Reference Base&lt;/em&gt; (2006)&lt;br /&gt;6 &amp;ndash; Correspondance des horizons entre syst&amp;egrave;mes CPCS et &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt;&lt;br /&gt;7 &amp;ndash; Correspondances possibles entre cat&amp;eacute;gories de la classification CPCS et &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008&lt;/em&gt;&lt;br /&gt;8 &amp;ndash; Possibilit&amp;eacute; de regroupement des GER en quatorze cat&amp;eacute;gories&lt;br /&gt;9 &amp;ndash; Lexique&lt;br /&gt;&lt;br /&gt;Liste des 110 r&amp;eacute;f&amp;eacute;rences du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008 &lt;/em&gt;(par chapitres)&lt;br /&gt;Liste des 110 r&amp;eacute;f&amp;eacute;rences du &lt;em&gt;R&amp;eacute;f&amp;eacute;rentiel p&amp;eacute;dologique 2008 &lt;/em&gt;(par ordre alphab&amp;eacute;tique)&lt;br /&gt;&amp;nbsp;&lt;/p&gt;</Text>
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