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1. | | TEODORO, K. B. R.; ALVARENGA, A. D.; OLIVEIRA, L. F. R.; CHAGAS, P. A. M.; LOPES. R. G.; ANDRE, R. S.; MERCANTE, L. A.; ALVES, F.; STRINGASCI, M. D.; BUZZA, H. H.; INADA, N. M.; CORREA, D. S. Fast Fabrication of Multifunctional PCL/Curcumin Nanofibrous Membranes for Wound Dressings. ACS Applied Bio Materials, v. 6, 2023. 2325–2337 Biblioteca(s): Embrapa Instrumentação. |
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2. | | FERREIRA, L. M. B.; ALONSO, J. D.; KIILL, C. P.; FERREIRA, N. N.; BUZZÁ, H. H.; GODOI, D. R. M. de; BRITTO, D. de; ASSIS, O. B. G. de; SERAPHIM, T. V.; BORGES, J. C.; GREMIÃO, M. P. D. Exploiting supramolecular interactions to produce bevacizumab-loaded nanoparticles for potential mucosal delivery. European Polymer Journal, v. 103, p. 238-250, jun. 2018. 238-250 Biblioteca(s): Embrapa Instrumentação; Embrapa Semiárido. |
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Registros recuperados : 2 | |
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Registro Completo
Biblioteca(s): |
Embrapa Solos. |
Data corrente: |
27/11/2017 |
Data da última atualização: |
10/09/2021 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 2 |
Autoria: |
FONTANA, A.; CHAGAS, C. da S.; DONAGEMMA, G. K.; MENEZES, A. R. de; CALDERANO FILHO, B. |
Afiliação: |
ADEMIR FONTANA, CNPS; CESAR DA SILVA CHAGAS, CNPS; GUILHERME KANGUSSU DONAGEMMA, CNPS; AMDRESSA ROSAS DE MENEZES, UFRRJ; BRAZ CALDERANO FILHO, CNPS. |
Título: |
Soils developed on geomorphic surfaces in the mountain region of the State of Rio de Janeiro. |
Ano de publicação: |
2017 |
Fonte/Imprenta: |
Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 41, p. 1-17, 2017. |
DOI: |
10.1590/18069657rbcs20160574 |
Idioma: |
Inglês |
Conteúdo: |
The evaluation of soils in representative landscapes constitutes an opportunity to evaluate spatial distribution, discuss formation processes, and apply this knowledge to land use and management. In this sense, from the perspective of an environmentally diversified region, the aim of the present study is to evaluate the occurrence and understand the formation of soils in different geomorphic surfaces of a landscape from a mountain region in the state of Rio de Janeiro. The study was developed in the Pito Aceso microbasin in the municipality of Bom Jardim, composed of narrow valleys and a rugged mountain domain, with elevation between 640 and 1,270 m. In a representative landscape, the geomorphic surfaces were obtained from the slope segments and flow lines. On the geomorphic surfaces, soil profiles were described by their morphological properties, collected, and analyzed to describe the chemical and physical properties of each horizon. Geomorphological aspects and possible variations of the parent material directly affected pedogenesis and led to distinct soil classes in the landscape. Variation in the geomorphic surfaces directs the processes for soil formation under current conditions, as well as the preservation of polygenetic soils. Soils of lower development and with greater participation of the exchangeable cations were identified at the summit (talus deposit) (Neossolo Litólico and Cambissolo Húmico) and toeslope (colluvial-alluvial) (Neossolo Flúvico), whereas more developed soils with lower nutrient content occur in the concave (Argissolos Vermelho and Amarelo) and convex (Latossolo Amarelo) backslope, except for the Argissolo Vermelho-Amarelo in the shoulder, which had high exchangeable cations contents. MenosThe evaluation of soils in representative landscapes constitutes an opportunity to evaluate spatial distribution, discuss formation processes, and apply this knowledge to land use and management. In this sense, from the perspective of an environmentally diversified region, the aim of the present study is to evaluate the occurrence and understand the formation of soils in different geomorphic surfaces of a landscape from a mountain region in the state of Rio de Janeiro. The study was developed in the Pito Aceso microbasin in the municipality of Bom Jardim, composed of narrow valleys and a rugged mountain domain, with elevation between 640 and 1,270 m. In a representative landscape, the geomorphic surfaces were obtained from the slope segments and flow lines. On the geomorphic surfaces, soil profiles were described by their morphological properties, collected, and analyzed to describe the chemical and physical properties of each horizon. Geomorphological aspects and possible variations of the parent material directly affected pedogenesis and led to distinct soil classes in the landscape. Variation in the geomorphic surfaces directs the processes for soil formation under current conditions, as well as the preservation of polygenetic soils. Soils of lower development and with greater participation of the exchangeable cations were identified at the summit (talus deposit) (Neossolo Litólico and Cambissolo Húmico) and toeslope (colluvial-alluvial) (Neossolo Flúvico), whereas more d... Mostrar Tudo |
Palavras-Chave: |
Classes de solos; Desenvolvimento pedogenético; Relação solo-paisagem. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/167548/1/2017-055.pdf
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Marc: |
LEADER 02463naa a2200217 a 4500 001 2080804 005 2021-09-10 008 2017 bl uuuu u00u1 u #d 024 7 $a10.1590/18069657rbcs20160574$2DOI 100 1 $aFONTANA, A. 245 $aSoils developed on geomorphic surfaces in the mountain region of the State of Rio de Janeiro.$h[electronic resource] 260 $c2017 520 $aThe evaluation of soils in representative landscapes constitutes an opportunity to evaluate spatial distribution, discuss formation processes, and apply this knowledge to land use and management. In this sense, from the perspective of an environmentally diversified region, the aim of the present study is to evaluate the occurrence and understand the formation of soils in different geomorphic surfaces of a landscape from a mountain region in the state of Rio de Janeiro. The study was developed in the Pito Aceso microbasin in the municipality of Bom Jardim, composed of narrow valleys and a rugged mountain domain, with elevation between 640 and 1,270 m. In a representative landscape, the geomorphic surfaces were obtained from the slope segments and flow lines. On the geomorphic surfaces, soil profiles were described by their morphological properties, collected, and analyzed to describe the chemical and physical properties of each horizon. Geomorphological aspects and possible variations of the parent material directly affected pedogenesis and led to distinct soil classes in the landscape. Variation in the geomorphic surfaces directs the processes for soil formation under current conditions, as well as the preservation of polygenetic soils. Soils of lower development and with greater participation of the exchangeable cations were identified at the summit (talus deposit) (Neossolo Litólico and Cambissolo Húmico) and toeslope (colluvial-alluvial) (Neossolo Flúvico), whereas more developed soils with lower nutrient content occur in the concave (Argissolos Vermelho and Amarelo) and convex (Latossolo Amarelo) backslope, except for the Argissolo Vermelho-Amarelo in the shoulder, which had high exchangeable cations contents. 653 $aClasses de solos 653 $aDesenvolvimento pedogenético 653 $aRelação solo-paisagem 700 1 $aCHAGAS, C. da S. 700 1 $aDONAGEMMA, G. K. 700 1 $aMENEZES, A. R. de 700 1 $aCALDERANO FILHO, B. 773 $tRevista Brasileira de Ciência do Solo, Viçosa, MG$gv. 41, p. 1-17, 2017.
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Registro original: |
Embrapa Solos (CNPS) |
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Biblioteca |
ID |
Origem |
Tipo/Formato |
Classificação |
Cutter |
Registro |
Volume |
Status |
Fechar
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Registro completo
Biblioteca(s): |
Catálogo Coletivo de Periódicos Embrapa; Embrapa Amazônia Oriental. |
Identificador: |
503 |
Data corrente: |
09/05/2002 |
Data da última atualização: |
12/05/2015 |
Código do título: |
0901372 |
ISSN: |
0100-1922 |
Código CCN: |
003459-2 |
Título e Subtítulo: |
ANAIS DA BIBLIOTECA NACIONAL |
Título alternativo: |
ANAES DA BIBLIOTHECA NACIONAL |
Entidade: |
Biblioteca Nacional do Rio de Janeiro |
Local de publicação: |
Rio De Janeiro, RJ |
Periodicidade: |
Anual |
Inicio de publicação: |
1876 |
Coleções da unidade: |
Embrapa Amazônia Oriental 1883 11; 1884/85 12; 1886 14(1-2); 1887/88 15(1/2); 1889/90 16(1-2); 1891/92 17; 1896 18; 1898 20; 1899 21; 1900 22; 1901 23; 1903 25; 1904 26; 1905 27; 1906 28; 1907 29; 1908 30; 1909 31; 1910 32; 1911 33; 1912 34; 1913 35; 1914 36; 1915 37; 1916 38; 1917 39; 1918 40; 1919 41; 1920 42; 1924 46; 1925 47; 1927 49; 1928 50; 1929 51; 1930 52; 1931 53; 1932 54; 1933 55; 1934 56; 1935 57; 1936 58; 1937 59; 1938 60; 1948 66, 67; 1949 68; 1950 69, 70; 1951 71, 72; 1953 74; 1954 73; 1955 75; 1956 76; 1957 77; 1958 78; 1959 79; 1960 80; 1962 82; 1963 83; 1964 84; 1965 85; 1966 86; 1967 87; 1968 88; 1969 89; 1970 90; 1971 91; 1972 92(3,6-8); 1973 93; 1974 94; 1975 95(1-2); 1976 96; 1977 97; 1978 98; 1980 100; 1981 101; 1982 102; 1983 103; 1985 105; 1986 106; 1987 107; 1988 108; 1989 109; 1990 110; 1991 111; 1992 112; 1993 113; 1994 114 Classificação: 981.05A6 |
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