FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2023320981> ?p ?o ?g. }

• W2023320981 endingPage "313" @default.
• W2023320981 startingPage "300" @default.
• W2023320981 abstract "Volcanic soils constitute an important resource for agriculture and forestry in Central Mexico, as well as in various world regions. They exhibit unique properties and high productive potential related to the amorphous materials they contain. The relationship between amorphous materials, soil characteristic and functioning, has not been well studied. The objectives of the present work were to assess the influence of land use (agricultural and forest), topography and other soil forming factors on physical, chemical and mineralogical characteristics and pedological processes responsible for soil genesis and soil classification of two volcanic soil profiles derived from andesitic parent material located 150 m away from each other within the same toposequences. The toposequence is located in the Trans-Mexican Volcanic Belt (TMVB), a highly populated region of Central Mexico that provides part of the water for Mexico City megapolis. A series of field and laboratory techniques including physical, chemical, micromorphological, X-ray diffraction (XRD), transmission electron microscopy (TEM), infra-red analysis, Mössbauer spectroscopy were used. The main factor affecting the present morphology of the soil profiles was the topography. The mineralogical features of the upper layers of the maize profile (Pachic Andosol), indicate redistribution of soil material from the upper part of the toposequence. The land use change favored this redistribution. Deeper horizons of this profile were developed from volcanic ashes deposited in situ. hematite and ferrihydrite, considered markers of evolution in redistributed soil material were observed in this profile associated with allophane. The presence of hematite has been reported for the first time in Mexican Andosols. The present characteristics of the forest profile (Dystric Cambisol) are mainly due to the pedological process of the volcanic ash layers remaining in situ after the redistribution and volcanic breccia. It was concluded that the forest profile evolved from an Andosol to an Inceptisol, which was evidenced by desaturation, loss of silica and organic carbon. In this profile the Fe minerals were associated with the presence of gibbsite and halloysite. The position in the toposequence and the physical and chemical characteristics of these profiles define their present functioning, such as losses by erosion and C dynamics." @default.
• W2023320981 created "2016-06-24" @default.
• W2023320981 creator A5012145548 @default.
• W2023320981 creator A5013263755 @default.
• W2023320981 creator A5027929837 @default.
• W2023320981 creator A5034531732 @default.
• W2023320981 creator A5044750338 @default.
• W2023320981 creator A5065635734 @default.
• W2023320981 creator A5065870430 @default.
• W2023320981 creator A5083384633 @default.
• W2023320981 date "2007-05-01" @default.
• W2023320981 modified "2023-09-30" @default.
• W2023320981 title "Characterization, functioning and classification of two volcanic soil profiles under different land uses in Central Mexico" @default.
• W2023320981 cites W1005764322 @default.
• W2023320981 cites W135820806 @default.
• W2023320981 cites W1476881749 @default.
• W2023320981 cites W1483206178 @default.
• W2023320981 cites W1524895157 @default.
• W2023320981 cites W1526771124 @default.
• W2023320981 cites W1565062102 @default.
• W2023320981 cites W1571810959 @default.
• W2023320981 cites W1583123053 @default.
• W2023320981 cites W1880078023 @default.
• W2023320981 cites W1969686739 @default.
• W2023320981 cites W1990328742 @default.
• W2023320981 cites W1991662480 @default.
• W2023320981 cites W1992824744 @default.
• W2023320981 cites W1992998140 @default.
• W2023320981 cites W1997224366 @default.
• W2023320981 cites W1998225761 @default.
• W2023320981 cites W1998886186 @default.
• W2023320981 cites W2010514376 @default.
• W2023320981 cites W2010696530 @default.
• W2023320981 cites W2012601928 @default.
• W2023320981 cites W2012784968 @default.
• W2023320981 cites W2017060194 @default.
• W2023320981 cites W2017652551 @default.
• W2023320981 cites W2020755275 @default.
• W2023320981 cites W2021341645 @default.
• W2023320981 cites W2029200698 @default.
• W2023320981 cites W2033025648 @default.
• W2023320981 cites W2035524507 @default.
• W2023320981 cites W203618391 @default.
• W2023320981 cites W2059751904 @default.
• W2023320981 cites W2066259824 @default.
• W2023320981 cites W2067257867 @default.
• W2023320981 cites W2070593972 @default.
• W2023320981 cites W2079386155 @default.
• W2023320981 cites W2081369590 @default.
• W2023320981 cites W2083097973 @default.
• W2023320981 cites W2092509324 @default.
• W2023320981 cites W2099176431 @default.
• W2023320981 cites W2131920195 @default.
• W2023320981 cites W2237939624 @default.
• W2023320981 cites W2269072506 @default.
• W2023320981 cites W2317474572 @default.
• W2023320981 cites W2324692134 @default.
• W2023320981 cites W2333832460 @default.
• W2023320981 cites W2940827091 @default.
• W2023320981 cites W2951098859 @default.
• W2023320981 cites W3009397686 @default.
• W2023320981 cites W69002474 @default.
• W2023320981 cites W946336681 @default.
• W2023320981 cites W2798947846 @default.
• W2023320981 doi "https://doi.org/10.1016/j.geoderma.2007.02.008" @default.
• W2023320981 hasPublicationYear "2007" @default.
• W2023320981 type Work @default.
• W2023320981 sameAs 2023320981 @default.
• W2023320981 citedByCount "32" @default.
• W2023320981 countsByYear W20233209812012 @default.
• W2023320981 countsByYear W20233209812013 @default.
• W2023320981 countsByYear W20233209812014 @default.
• W2023320981 countsByYear W20233209812015 @default.
• W2023320981 countsByYear W20233209812016 @default.
• W2023320981 countsByYear W20233209812018 @default.
• W2023320981 countsByYear W20233209812019 @default.
• W2023320981 countsByYear W20233209812020 @default.
• W2023320981 countsByYear W20233209812022 @default.
• W2023320981 crossrefType "journal-article" @default.
• W2023320981 hasAuthorship W2023320981A5012145548 @default.
• W2023320981 hasAuthorship W2023320981A5013263755 @default.
• W2023320981 hasAuthorship W2023320981A5027929837 @default.
• W2023320981 hasAuthorship W2023320981A5034531732 @default.
• W2023320981 hasAuthorship W2023320981A5044750338 @default.
• W2023320981 hasAuthorship W2023320981A5065635734 @default.
• W2023320981 hasAuthorship W2023320981A5065870430 @default.
• W2023320981 hasAuthorship W2023320981A5083384633 @default.
• W2023320981 hasConcept C120806208 @default.
• W2023320981 hasConcept C127313418 @default.
• W2023320981 hasConcept C150394285 @default.
• W2023320981 hasConcept C152494472 @default.
• W2023320981 hasConcept C159390177 @default.
• W2023320981 hasConcept C159750122 @default.
• W2023320981 hasConcept C17409809 @default.
• W2023320981 hasConcept C178790620 @default.
• W2023320981 hasConcept C184269829 @default.
• W2023320981 hasConcept C185592680 @default.
• W2023320981 hasConcept C192241223 @default.

• next