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Catálogo Taxonômico da Fauna do Brasil: Setting the baseline knowledge on the animal diversity in Brazil Brasil
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Boeger, Walter A.
; Valim, Michel P.
; Zaher, Hussam
; Rafael, José A.
; Forzza, Rafaela C.
; Percequillo, Alexandre R.
; Serejo, Cristiana S.
; Garraffoni, André R.S.
; Santos, Adalberto J.
; Slipinski, Adam
; Linzmeier, Adelita M.
; Calor, Adolfo R.
; Garda, Adrian A.
; Kury, Adriano B.
; Fernandes, Agatha C.S.
; Agudo-Padrón, Aisur I.
; Akama, Alberto
; Silva Neto, Alberto M. da
; Burbano, Alejandro L.
; Menezes, Aleksandra
; Pereira-Colavite, Alessandre
; Anichtchenko, Alexander
; Lees, Alexander C.
; Bezerra, Alexandra M.R.
; Domahovski, Alexandre C.
; Pimenta, Alexandre D.
; Aleixo, Alexandre L.P.
; Marceniuk, Alexandre P.
; Paula, Alexandre S. de
; Somavilla, Alexandre
; Specht, Alexandre
; Camargo, Alexssandro
; Newton, Alfred F.
; Silva, Aline A.S. da
; Santos, Aline B. dos
; Tassi, Aline D.
; Aragão, Allan C.
; Santos, Allan P.M.
; Migotto, Alvaro E.
; Mendes, Amanda C.
; Cunha, Amanda
; Chagas Júnior, Amazonas
; Sousa, Ana A.T. de
; Pavan, Ana C.
; Almeida, Ana C.S.
; Peronti, Ana L.B.G.
; Henriques-Oliveira, Ana L.
; Prudente, Ana L.
; Tourinho, Ana L.
; Pes, Ana M.O.
; Carmignotto, Ana P.
; Wengrat, Ana P.G. da Silva
; Dornellas, Ana P.S.
; Molin, Anamaria Dal
; Puker, Anderson
; Morandini, André C.
; Ferreira, André da S.
; Martins, André L.
; Esteves, André M.
; Fernandes, André S.
; Roza, André S.
; Köhler, Andreas
; Paladini, Andressa
; Andrade, Andrey J. de
; Pinto, Ângelo P.
; Salles, Anna C. de A.
; Gondim, Anne I.
; Amaral, Antonia C.Z.
; Rondón, Antonio A.A.
; Brescovit, Antonio
; Lofego, Antônio C.
; Marques, Antonio C.
; Macedo, Antonio
; Andriolo, Artur
; Henriques, Augusto L.
; Ferreira Júnior, Augusto L.
; Lima, Aurino F. de
; Barros, Ávyla R. de A.
; Brito, Ayrton do R.
; Romera, Bárbara L.V.
; Vasconcelos, Beatriz M.C. de
; Frable, Benjamin W.
; Santos, Bernardo F.
; Ferraz, Bernardo R.
; Rosa, Brunno B.
; Sampaio, Brunno H.L.
; Bellini, Bruno C.
; Clarkson, Bruno
; Oliveira, Bruno G. de
; Corrêa, Caio C.D.
; Martins, Caleb C.
; Castro-Guedes, Camila F. de
; Souto, Camilla
; Bicho, Carla de L.
; Cunha, Carlo M.
; Barboza, Carlos A. de M.
; Lucena, Carlos A.S. de
; Barreto, Carlos
; Santana, Carlos D.C.M. de
; Agne, Carlos E.Q.
; Mielke, Carlos G.C.
; Caetano, Carlos H.S.
; Flechtmann, Carlos H.W.
; Lamas, Carlos J.E.
; Rocha, Carlos
; Mascarenhas, Carolina S.
; Margaría, Cecilia B.
; Waichert, Cecilia
; Digiani, Celina
; Haddad, Célio F.B.
; Azevedo, Celso O.
; Benetti, Cesar J.
; Santos, Charles M.D. dos
; Bartlett, Charles R.
; Bonvicino, Cibele
; Ribeiro-Costa, Cibele S.
; Santos, Cinthya S.G.
; Justino, Cíntia E.L.
; Canedo, Clarissa
; Bonecker, Claudia C.
; Santos, Cláudia P.
; Carvalho, Claudio J.B. de
; Gonçalves, Clayton C.
; Galvão, Cleber
; Costa, Cleide
; Oliveira, Cléo D.C. de
; Schwertner, Cristiano F.
; Andrade, Cristiano L.
; Pereira, Cristiano M.
; Sampaio, Cristiano
; Dias, Cristina de O.
; Lucena, Daercio A. de A.
; Manfio, Daiara
; Amorim, Dalton de S.
; Queiroz, Dalva L. de
; Queiroz, Dalva L. de
; Colpani, Daniara
; Abbate, Daniel
; Aquino, Daniel A.
; Burckhardt, Daniel
; Cavallari, Daniel C.
; Prado, Daniel de C. Schelesky
; Praciano, Daniel L.
; Basílio, Daniel S.
; Bená, Daniela de C.
; Toledo, Daniela G.P. de
; Takiya, Daniela M.
; Fernandes, Daniell R.R.
; Ament, Danilo C.
; Cordeiro, Danilo P.
; Silva, Darliane E.
; Pollock, Darren A.
; Muniz, David B.
; Gibson, David I.
; Nogueira, David S.
; Marques, Dayse W.A.
; Lucatelli, Débora
; Garcia, Deivys M.A.
; Baêta, Délio
; Ferreira, Denise N.M.
; Rueda-Ramírez, Diana
; Fachin, Diego A.
; Souza, Diego de S.
; Rodrigues, Diego F.
; Pádua, Diego G. de
; Barbosa, Diego N.
; Dolibaina, Diego R.
; Amaral, Diogo C.
; Chandler, Donald S.
; Maccagnan, Douglas H.B.
; Caron, Edilson
; Carvalho, Edrielly
; Adriano, Edson A.
; Abreu Júnior, Edson F. de
; Pereira, Edson H.L.
; Viegas, Eduarda F.G.
; Carneiro, Eduardo
; Colley, Eduardo
; Eizirik, Eduardo
; Santos, Eduardo F. dos
; Shimbori, Eduardo M.
; Suárez-Morales, Eduardo
; Arruda, Eliane P. de
; Chiquito, Elisandra A.
; Lima, Élison F.B.
; Castro, Elizeu B. de
; Orlandin, Elton
; Nascimento, Elynton A. do
; Razzolini, Emanuel
; Gama, Emanuel R.R.
; Araujo, Enilma M. de
; Nishiyama, Eric Y.
; Spiessberger, Erich L.
; Santos, Érika C.L. dos
; Contreras, Eugenia F.
; Galati, Eunice A.B.
; Oliveira Junior, Evaldo C. de
; Gallardo, Fabiana
; Hernandes, Fabio A.
; Lansac-Tôha, Fábio A.
; Pitombo, Fabio B.
; Dario, Fabio Di
; Santos, Fábio L. dos
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; Nascimento, Fabio O. do
; Olmos, Fabio
; Amaral, Fabio R.
; Schunck, Fabio
; Godoi, Fábio S. P. de
; Machado, Fabrizio M.
; Barbo, Fausto E.
; Agrain, Federico A.
; Ribeiro, Felipe B.
; Moreira, Felipe F.F.
; Barbosa, Felipe F.
; Silva, Fenanda S.
; Cavalcanti, Fernanda F.
; Straube, Fernando C.
; Carbayo, Fernando
; Carvalho Filho, Fernando
; Zanella, Fernando C.V.
; Jacinavicius, Fernando de C.
; Farache, Fernando H.A.
; Leivas, Fernando
; Dias, Fernando M.S.
; Mantellato, Fernando
; Vaz-de-Mello, Fernando Z.
; Gudin, Filipe M.
; Albuquerque, Flávio
; Molina, Flavio B.
; Passos, Flávio D.
; Shockley, Floyd W.
; Pinheiro, Francielly F.
; Mello, Francisco de A.G. de
; Nascimento, Francisco E. de L.
; Franco, Francisco L.
; Oliveira, Francisco L. de
; Melo, Francisco T. de V.
; Quijano, Freddy R.B.
; Salles, Frederico F.
; Biffi, Gabriel
; Queiroz, Gabriel C.
; Bizarro, Gabriel L.
; Hrycyna, Gabriela
; Leviski, Gabriela
; Powell, Gareth S.
; Santos, Geane B. dos
; Morse, Geoffrey E.
; Brown, George
; Mattox, George M.T.
; Zimbrão, Geraldo
; Carvalho, Gervásio S.
; Miranda, Gil F.G.
; Moraes, Gilberto J. de
; Lourido, Gilcélia M.
; Neves, Gilmar P.
; Moreira, Gilson R.P.
; Montingelli, Giovanna G.
; Maurício, Giovanni N.
; Marconato, Gláucia
; Lopez, Guilherme E.L.
; Silva, Guilherme L. da
; Muricy, Guilherme
; Brito, Guilherme R.R.
; Garbino, Guilherme S.T.
; Flores, Gustavo E.
; Graciolli, Gustavo
; Libardi, Gustavo S.
; Proctor, Heather C.
; Gil-Santana, Helcio R.
; Varella, Henrique R.
; Escalona, Hermes E.
; Schmitz, Hermes J.
; Rodrigues, Higor D.D.
; Galvão Filho, Hilton de C.
; Quintino, Hingrid Y.S.
; Pinto, Hudson A.
; Rainho, Hugo L.
; Miyahira, Igor C.
; Gonçalves, Igor de S.
; Martins, Inês X.
; Cardoso, Irene A.
; Oliveira, Ismael B. de
; Franz, Ismael
; Fernandes, Itanna O.
; Golfetti, Ivan F.
; S. Campos-Filho, Ivanklin
; Oliveira, Ivo de S.
; Delabie, Jacques H.C.
; Oliveira, Jader de
; Prando, Jadila S.
; Patton, James L.
; Bitencourt, Jamille de A.
; Silva, Janaina M.
; Santos, Jandir C.
; Arruda, Janine O.
; Valderrama, Jefferson S.
; Dalapicolla, Jeronymo
; Oliveira, Jéssica P.
; Hájek, Jiri
; Morselli, João P.
; Narita, João P.
; Martin, João P.I.
; Grazia, Jocélia
; McHugh, Joe
; Cherem, Jorge J.
; Farias Júnior, José A.S.
; Fernandes, Jose A.M.
; Pacheco, José F.
; Birindelli, José L.O.
; Rezende, José M.
; Avendaño, Jose M.
; Duarte, José M. Barbanti
; Ribeiro, José R. Inácio
; Mermudes, José R.M.
; Pujol-Luz, José R.
; Santos, Josenilson R. dos
; Câmara, Josenir T.
; Teixeira, Joyce A.
; Prado, Joyce R. do
; Botero, Juan P.
; Almeida, Julia C.
; Kohler, Julia
; Gonçalves, Julia P.
; Beneti, Julia S.
; Donahue, Julian P.
; Alvim, Juliana
; Almeida, Juliana C.
; Segadilha, Juliana L.
; Wingert, Juliana M.
; Barbosa, Julianna F.
; Ferrer, Juliano
; Santos, Juliano F. dos
; Kuabara, Kamila M.D.
; Nascimento, Karine B.
; Schoeninger, Karine
; Campião, Karla M.
; Soares, Karla
; Zilch, Kássia
; Barão, Kim R.
; Teixeira, Larissa
; Sousa, Laura D. do N.M. de
; Dumas, Leandro L.
; Vieira, Leandro M.
; Azevedo, Leonardo H.G.
; Carvalho, Leonardo S.
; Souza, Leonardo S. de
; Rocha, Leonardo S.G.
; Bernardi, Leopoldo F.O.
; Vieira, Letícia M.
; Johann, Liana
; Salvatierra, Lidianne
; Oliveira, Livia de M.
; Loureiro, Lourdes M.A. El-moor
; Barreto, Luana B.
; Barros, Luana M.
; Lecci, Lucas
; Camargos, Lucas M. de
; Lima, Lucas R.C.
; Almeida, Lucia M.
; Martins, Luciana R.
; Marinoni, Luciane
; Moura, Luciano de A.
; Lima, Luciano
; Naka, Luciano N.
; Miranda, Lucília S.
; Salik, Lucy M.
; Bezerra, Luis E.A.
; Silveira, Luis F.
; Campos, Luiz A.
; Castro, Luiz A.S. de
; Pinho, Luiz C.
; Silveira, Luiz F.L.
; Iniesta, Luiz F.M.
; Tencatt, Luiz F.C.
; Simone, Luiz R.L.
; Malabarba, Luiz R.
; Cruz, Luiza S. da
; Sekerka, Lukas
; Barros, Lurdiana D.
; Santos, Luziany Q.
; Skoracki, Maciej
; Correia, Maira A.
; Uchoa, Manoel A.
; Andrade, Manuella F.G.
; Hermes, Marcel G.
; Miranda, Marcel S.
; Araújo, Marcel S. de
; Monné, Marcela L.
; Labruna, Marcelo B.
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; Duarte, Marcelo
; Knoff, Marcelo
; Nogueira, Marcelo
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; Carvalho, Marcelo R. de
; Tavares, Marcelo T.
; Kitahara, Marcelo V.
; Justo, Marcia C.N.
; Botelho, Marcia J.C.
; Couri, Márcia S.
; Borges-Martins, Márcio
; Felix, Márcio
; Oliveira, Marcio L. de
; Bologna, Marco A.
; Gottschalk, Marco S.
; Tavares, Marcos D.S.
; Lhano, Marcos G.
; Bevilaqua, Marcus
; Santos, Marcus T.T.
; Domingues, Marcus V.
; Sallum, Maria A.M.
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; Bartz, Marie L.C.
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; Martins, Maurício L.
; Segura, Melissa O.
; Cardenas, Melissa Q.
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; Monné, Miguel A.
; Casagrande, Mirna M.
; Fernandez, Monica A.
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; Evangelista, Olivia
; Shibatta, Oscar A.
; Oliveira, Otto M.P.
; Albornoz, Pablo C.L.
; Dellapé, Pablo M.
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; Shimabukuro, Paloma H.F.
; Grossi, Paschoal
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; Lima, Patricia O.V.
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; Silva, Paula K.R.
; Riccardi, Paula R.
; Garcia, Paulo C. de A.
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; Corgosinho, Paulo H.C.
; Lucinda, Paulo
; Costa, Paulo M.S.
; Alves, Paulo P.
; Roth, Paulo R. de O.
; Coelho, Paulo R.S.
; Duarte, Paulo R.M.
; Carvalho, Pedro F. de
; Gnaspini, Pedro
; Souza-Dias, Pedro G.B.
; Linardi, Pedro M.
; Bartholomay, Pedro R.
; Demite, Peterson R.
; Bulirsch, Petr
; Boll, Piter K.
; Pereira, Rachel M.M.
; Silva, Rafael A.P.F.
; Moura, Rafael B. de
; Boldrini, Rafael
; Silva, Rafaela A. da
; Falaschi, Rafaela L.
; Cordeiro, Ralf T.S.
; Mello, Ramon J.C.L.
; Singer, Randal A.
; Querino, Ranyse B.
; Heleodoro, Raphael A.
; Castilho, Raphael de C.
; Constantino, Reginaldo
; Guedes, Reinaldo C.
; Carrenho, Renan
; Gomes, Renata S.
; Gregorin, Renato
; Machado, Renato J.P.
; Bérnils, Renato S.
; Capellari, Renato S.
; Silva, Ricardo B.
; Kawada, Ricardo
; Dias, Ricardo M.
; Siewert, Ricardo
; Brugnera, Ricaro
; Leschen, Richard A.B.
; Constantin, Robert
; Robbins, Robert
; Pinto, Roberta R.
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; Salvador, Rodrigo B.
; Marques, Rodrigo C.
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; Dios, Rodrigo de V.P.
; Johnsson, Rodrigo
; Feitosa, Rodrigo M.
; Hutchings, Roger W.
; Lara, Rogéria I.R.
; Rossi, Rogério V.
; Gerstmeier, Roland
; Ochoa, Ronald
; Hutchings, Rosa S.G.
; Ale-Rocha, Rosaly
; Rocha, Rosana M. da
; Tidon, Rosana
; Brito, Rosangela
; Pellens, Roseli
; Santos, Sabrina R. dos
; Santos, Sandra D. dos
; Paiva, Sandra V.
; Santos, Sandro
; Oliveira, Sarah S. de
; Costa, Sávio C.
; Gardner, Scott L.
; Leal, Sebastián A. Muñoz
; Aloquio, Sergio
; Bonecker, Sergio L.C.
; Bueno, Sergio L. de S.
; Almeida, Sérgio M. de
; Stampar, Sérgio N.
; Andena, Sérgio R.
; Posso, Sergio R.
; Lima, Sheila P.
; Gadelha, Sian de S.
; Thiengo, Silvana C.
; Cohen, Simone C.
; Brandão, Simone N.
; Rosa, Simone P.
; Ribeiro, Síria L.B.
; Letana, Sócrates D.
; Santos, Sonia B. dos
; Andrade, Sonia C.S.
; Dávila, Stephane
; Vaz, Stéphanie
; Peck, Stewart B.
; Christo, Susete W.
; Cunha, Suzan B.Z.
; Gomes, Suzete R.
; Duarte, Tácio
; Madeira-Ott, Taís
; Marques, Taísa
; Roell, Talita
; Lima, Tarcilla C. de
; Sepulveda, Tatiana A.
; Maria, Tatiana F.
; Ruschel, Tatiana P.
; Rodrigues, Thaiana
; Marinho, Thais A.
; Almeida, Thaís M. de
; Miranda, Thaís P.
; Freitas, Thales R.O.
; Pereira, Thalles P.L.
; Zacca, Thamara
; Pacheco, Thaynara L.
; Martins, Thiago F.
; Alvarenga, Thiago M.
; Carvalho, Thiago R. de
; Polizei, Thiago T.S.
; McElrath, Thomas C.
; Henry, Thomas
; Pikart, Tiago G.
; Porto, Tiago J.
; Krolow, Tiago K.
; Carvalho, Tiago P.
; Lotufo, Tito M. da C.
; Caramaschi, Ulisses
; Pinheiro, Ulisses dos S.
; Pardiñas, Ulyses F.J.
; Maia, Valéria C.
; Tavares, Valeria
; Costa, Valmir A.
; Amaral, Vanessa S. do
; Silva, Vera C.
; Wolff, Vera R. dos S.
; Slobodian, Verônica
; Silva, Vinícius B. da
; Espíndola, Vinicius C.
; Costa-Silva, Vinicius da
; Bertaco, Vinicius de A.
; Padula, Vinícius
; Ferreira, Vinicius S.
; Silva, Vitor C.P. da
; Piacentini, Vítor de Q.
; Sandoval-Gómez, Vivian E.
; Trevine, Vivian
; Sousa, Viviane R.
; Sant’Anna, Vivianne B. de
; Mathis, Wayne N.
; Souza, Wesley de O.
; Colombo, Wesley D.
; Tomaszewska, Wioletta
; Wosiacki, Wolmar B.
; Ovando, Ximena M.C.
; Leite, Yuri L.R.
.
ABSTRACT The limited temporal completeness and taxonomic accuracy of species lists, made available in a traditional manner in scientific publications, has always represented a problem. These lists are invariably limited to a few taxonomic groups and do not represent up-to-date knowledge of all species and classifications. In this context, the Brazilian megadiverse fauna is no exception, and the Catálogo Taxonômico da Fauna do Brasil (CTFB) (http://fauna.jbrj.gov.br/), made public in 2015, represents a database on biodiversity anchored on a list of valid and expertly recognized scientific names of animals in Brazil. The CTFB is updated in near real time by a team of more than 800 specialists. By January 1, 2024, the CTFB compiled 133,691 nominal species, with 125,138 that were considered valid. Most of the valid species were arthropods (82.3%, with more than 102,000 species) and chordates (7.69%, with over 11,000 species). These taxa were followed by a cluster composed of Mollusca (3,567 species), Platyhelminthes (2,292 species), Annelida (1,833 species), and Nematoda (1,447 species). All remaining groups had less than 1,000 species reported in Brazil, with Cnidaria (831 species), Porifera (628 species), Rotifera (606 species), and Bryozoa (520 species) representing those with more than 500 species. Analysis of the CTFB database can facilitate and direct efforts towards the discovery of new species in Brazil, but it is also fundamental in providing the best available list of valid nominal species to users, including those in science, health, conservation efforts, and any initiative involving animals. The importance of the CTFB is evidenced by the elevated number of citations in the scientific literature in diverse areas of biology, law, anthropology, education, forensic science, and veterinary science, among others. publications problem uptodate up date classifications context exception (CTFB http//fauna.jbrj.gov.br/, httpfaunajbrjgovbr http //fauna.jbrj.gov.br/ , jbrj gov br (http://fauna.jbrj.gov.br/) 2015 Brazil 80 specialists 1 2024 133691 133 691 133,69 125138 125 138 125,13 82.3%, 823 82 3 (82.3% 102000 102 000 102,00 7.69%, 769 7 69 (7.69% 11000 11 11,00 . 3,567 3567 567 (3,56 2,292 2292 2 292 (2,29 1,833 1833 833 (1,83 1,447 1447 447 (1,44 1000 1,00 831 (83 628 (62 606 (60 520 (52 50 users science health biology law anthropology education others http//fauna.jbrj.gov.br/ faunajbrjgovbr //fauna.jbrj.gov.br (http://fauna.jbrj.gov.br/ 201 8 202 13369 13 133,6 12513 12 125,1 82.3% (82.3 10200 10 00 102,0 7.69% 76 6 (7.69 1100 11,0 3,56 356 56 (3,5 2,29 229 29 (2,2 1,83 183 83 (1,8 1,44 144 44 (1,4 100 1,0 (8 62 (6 60 52 (5 5 http//fauna.jbrj.gov.br (http://fauna.jbrj.gov.br 20 1336 133, 1251 125, 82.3 (82. 1020 0 102, 7.69 (7.6 110 11, 3,5 35 (3, 2,2 22 (2, 1,8 18 (1, 1,4 14 4 ( 82. (82 7.6 (7. 3, (3 2, (2 (1 7. (7
2.
Relationship between early age at menarche, older age at menopause and subtypes of breast cancer: a scoping review menarche cancer
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Lopes, Lucas Casagrande Passoni
; Medeiros, Gabriel Araújo
; Gualberto, Igor José Nogueira
; Gut, Thales Baptista
; Ferrazini, Rafael Vasconcelos Silva
; Negrato, Carlos Antonio
.
Abstract Objective To determine the relationship between early age at menarche, late age at menopause with specific subtypes of breast cancer (BC). Methods A literature search was conducted in Embase, Lilacs, PubMed, Scopus, and Scielo databases, following the Joanna Briggs Institute scoping review protocol and answering the question “How early age at menarche or late age at menopause are related to different breast cancer subtypes?”. Results A number of 4,003 studies were identified, of which 17 were selected. Most of the included articles found a clear relationship between early menarche, late menopause and some subtypes of BC, mainly, PR+, ER+, luminal, and HER-2 tumors. However, some studies have found a contradictory relationship and one study didn’t find any relationship between them. Conclusion A relationship between early age at menarche and advanced age at menopause was observed with some subtypes of breast cancer, since other factors must be considered in its understanding. BC. BC . (BC) Embase Lilacs PubMed Scopus databases How subtypes. subtypes?” 4003 4 003 4,00 identified 1 selected mainly PR PR+ ER ER+ luminal HER2 HER 2 HER- tumors However didnt didn t them understanding (BC subtypes? 400 00 4,0 40 0 4,
3.
Phosphorus acquisition from phosphate rock by soil cover crops, maize, and a buckwheat–maize cropping system
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Lopes, Valéria Adriele
; Wei, Marcelo Chan Fu
; Cardoso, Tainá Martins
; Martins, Eder de Souza
; Casagrande, José Carlos
; Mariano, Eduardo Dal’Ava
.
ABSTRACT Alternatives to enhance the consensual low phosphorus (P) use efficiency of agriculture may include use of phosphate rock (PR) and plant species with unequal ability to get soil and rock P interplanted in cropping systems to allow plants with higher ability to facilitate access to P of plants with lower ability. This study investigated (i) the maize and three soil cover crops on their capacity to acquire P from PR and (ii) measured P acquisition of maize interplanted with the soil cover crop with the highest capacity to acquire P shown in (i). Experiments were carried out in a greenhouse, with plants grown in single and mixed cropping in pots containing a sandy, low–P soil amended with Monocalcium Phosphate (McP) or the Brazilian PR Itafós. Plant biomass production with PR, in relation to McP, was 83.7 % for buckwheat, 83.6 % for forage radish, 51.8 % for maize, and 0.3 % for pigeon pea. Buckwheat showed capacity of acquiring P from PR; nevertheless, it did not increase growth or P nutrition of maize interplanted in the soil amended with PR, showing no significant P facilitation. The soil amended with McP showed competition between the two plants in the pots. Maize had a greater growth in mixed than in single cropping and this occurred at the expenses of buckwheat. Despite the P mobilization potential of buckwheat, its simple interplanting with maize did not produce positive results.
https://doi.org/10.1590/1678-992x-2020-0319
213 downloads
4.
Twenty-five-centimeter pre-grazing canopy height in palisade grass and forage peanut
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Ferreira, Igor Machado
; Homem, Bruno Grossi Costa
; Lima, Italo Braz Gonçalves de
; Dubeux Junior, José Carlos Batista
; Bernardes, Thiago Fernandes
; Danés, Marina de Arruda Camargo
; Casagrande, Daniel Rume
.
ABSTRACT: Short-term grazing behavior variables are sensitive to the canopy structure and have an impact on daily forage intake. This study evaluated the effect of pre- and post-grazing canopy heights on the forage harvesting process at a patch scale in a mixture of Brachiaria brizantha (Hochst. ex A. Rich.) Stapf. syn. Urochloa brizantha R.D. Webster cv. Marandu (palisade grass) and Arachis pintoi Krapov. & W.C. Greg. cv. Belomonte (forage peanut). Treatments were allocated to a split-plot arrangement in a completely randomized design. The plots, in their entirety, consisted of two pre-grazing canopy heights: 25 cm (CH25) and 35 cm (CH35); subplots consisted of three levels of defoliation severity: no defoliation (DS0); 20% depletion of pre-grazing canopy height (DS20); and 40% depletion of pre-grazing canopy height (DS40), with eight replications. Heifers were allowed to graze the patches (0.7 × 0.7 m) and their grazing behavior was recorded. Canopy structure measurements were taken both before and after grazing. Patches from CH35 presented greater stem mass for grass (p = 0.001) and legume (p = 0.002) than did patches from CH25. Bite rate, bite mass and instantaneous intake rate were greater for CH25 than for CH35 (p < 0.001, p = 0.068, and p = 0.074), and bite mass and instantaneous intake rate were lower for DS20 compared to DS0 (p = 0.032 and p = 0.016). Greater stem mass in the grazing strata negatively influenced the instantaneous intake rate.
https://doi.org/10.1590/1678-992x-2020-0090
232 downloads
5.
Environmental filters structure plant communities in the Brazilian Chaco
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Assunção, Vivian Almeida
; Silva, Danilo Muniz da
; Dalponti, Guilherme
; Sartori, Ângela Lúcia Bagnatori
; Casagrande, José Carlos
; Mansano, Vidal de Freitas
.
ABSTRACT We characterized taxonomic and functional differences between two vegetation physiognomies in the Brazilian Chaco, namely chaco woodland (CW) and chaco forest (CF), in order to understand which abiotic and biotic mechanisms underlie the establishment of different physiognomies. We characterized the vegetation physiognomies by comparing woody species composition, richness and diversity and functional diversity between CW and CF plots. We also measured soil variables to characterize abiotic factors related to the different physiognomies. Species richness and diversity and soil nutrient values were higher in CF. Leaf succulence and nitrogen content were higher in CW, while height, leaf area, and specific leaf area were higher in CF. The standardized effect size (SES) of functional richness was higher in CW, but the SES of functional dispersion did not differ between CF and CW. We observed a diversity gradient related to soil fertility. Traits of species in CW were related to adaptations to poor soils, while in CF floristic composition showed a prevalence of species with more attributes related to competition for light. Thus, the structure of the floristic community in CW is likely related to an environmental filter, while competition for resources prevails in CF.
https://doi.org/10.1590/0102-33062020abb0205
381 downloads
6.
Species representativeness of Fabaceae in restrictive soils explains the difference in structure of two types of Chaco vegetation
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Baptista, Mozart Sávio Pires
; Assunção, Vivian Almeida
; Bueno, Marcelo Leandro
; Casagrande, José Carlos
; Sartori, Ângela Lúcia Bagnatori
.
ABSTRACT The distributions of species of Fabaceae are strongly related to the soil. Their presence can alter restrictive conditions and favour the establishment of other species. However, it is still not known how the relationship between species of Fabaceae and edaphic factors interact in structuring woody Chaco vegetation. In this context, we aimed to test the hypothesis that restrictive edaphic conditions can explain the difference in floristic patterns of two types of vegetation through their species representativeness of Fabaceae. We analysed floristic consistency between wooded and forested Chaco to address how spatial and environment components might explain differences between them along with the effects of the interaction between Fabaceae and the soil. We observed that the association between environmental and spatial variables was more important than any individual factor in explaining the structuring of the communities. Both the percentage of species of Fabaceae present and the soil influence the structure of the two types of vegetation. Species of Fabaceae have greater potential as indicators in the wooded Chaco. Therefore, we suggest the interaction between soil types and species of Fabaceae plays a role during the structuring of the communities through the establishment of these species in more restrictive soils.
https://doi.org/10.1590/0102-33062020abb0064
667 downloads
7.
ESTOQUE DE CARBONO DE LATOSSOLOS EM SISTEMAS DE MANEJO NATURAL E ALTERADO
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Freitas, Ludmila de
; Oliveira, Ivanildo Amorim de
; Casagrande, José Carlos
; Silva, Laércio Santos
; Campos, Milton César Costa
.
RESUMO A conversão da condição natural do solo para a agricultura, em destaque para a monocultura de cana-deaçúcar impõe alterações nos atributos do solo. O objetivo do trabalho foi avaliar a variação do estoque de carbono de Latossolos com mata nativa, cana-de-açúcar e área reflorestada adjacentes, no município de Guariba - SP. Em cada área, foram coletadas, aleatoriamente, quatro amostras (compostas por quinze pontos), nas camadas de 0,0-0,10 e de 0,10-0,20 m. Foram avaliados os atributos densidade do solo, porosidade total, granulometria, teor de matéria orgânica, carbono orgânico total e estoque de carbono total no solo, de cada amostra nas duas profundidades estudadas. Os dados foram submetidos à análise de variância, correlação linear e análises multivariadas. Os resultados indicam que os teores de carbono são maiores nas camadas superficiais nas três áreas, decrescendo em profundidade. O solo da área de mata nativa apresenta o maior estoque de carbono, com 20,65 Mg ha-1, seguido pelo reflorestamento e cultivo de cana-de-açúcar, com 15,93 e 13,71 Mg ha-1, respectivamente, na profundidade de 0,0-0,10 m e 17,71 Mg ha-1, seguido pelo reflorestamento e cultivo de cana-de-açúcar, com 14,86 e 12,06 Mg ha-1, respectivamente, na profundidade de 0,10-0,20 m. Foi possível verificar tendo como referência a mata nativa, a perda de carbono no solo, sendo a área reflorestada e cultivada com cana-de-açúcar, na ordem de 22,9 e 33,6 %, na profundidade de 0,0-0,10 m e de 31,9 e 16,1 % nas áreas reflorestada e cultivada com cana-de-açúcar na profundidade de 0,10-0,20 m, respectivamente. Assim, conclui-se que intervenção humana através de práticas agropecuárias reduz o estoque de carbono no solo a patamares inferiores ao encontrado em condições de mata nativa.
ABSTRACT The natural condition conversion of the soil to agriculture, highlighting to the sugarcane monoculture, imposes changes in the soil attributes. This work aimed to evaluate the variation of the carbon storage of Oxisols under native forest, sugarcane, and adjacent reforested area, in Guariba, SP state. In each area, four samples (composed of fifteen points) were randomly collected, at 0.0-0.10 and 0.10-0.20 m layers. We evaluated soil density, total porosity, grain size, organic matter content, total organic carbon, and total soil carbon storage of each sample, at 0.0-0.10 and 0.10-0.20 m. Data were submitted to analysis of variance, linear correlation, and multivariate analyzes. The results indicate that the carbon content is higher in the superficial layers in all three areas, decreasing in depth. The soil of the native forest area has the highest carbon storage, 20.65 Mg ha-1, followed by reforestation and sugarcane cultivation areas, 15.93 and 13.71 Mg ha-1 respectively at 0.0-0.10 m, and 17.71 Mg ha-1, followed by reforestation and sugarcane cultivation areas, 14.86 and 12.06 Mg ha-1 respectively at 0.10 -0.20 m. It was possible to verify, comparing to the native forest, the loss of carbon in the soil, losses of 22.9 and 33.6% in the reforested and cultivated with sugar cane areas, at 0.0-0, 10 m, and 31.9 and 16.1% in the reforested and cultivated with sugarcane areas at 0.10-0.20 m, respectively. Thus, we may conclude that the human intervention through agricultural practices reduces the carbon storage in the soil at lower levels than the ones found in native forest conditions.
https://doi.org/10.5902/1980509831575
1823 downloads
8.
Nickel adsorption and desorption in an acric oxisol as a function of pH, ionic strength and incubation time
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RESUMO Apesar de o níquel (Ni) ser um elemento importante no ambiente, tanto pelo seu potencial benéfico, como tóxico, informações sobre o seu comportamento em solos tropicais são escassas. Reações de adsorção-dessorção de Ni em amostras superficias e subsuperficias de um Latossolo ácrico foram estudadas em três valores de pH do solo, variando de 3,0 a 8,0. Isotermas de adsorção-dessorção foram elaboradas a partir de experimentos com concentrações crescentes de Ni (5 a 100 mg L-1), durante 0, 4 e 12 semanas, usando CaCl2 0.01 e 0.1 M como eletrólito suporte para verificar o efeito do tempo de contato e da força iônica sobre a reação. Resultados experimentais foram adequadamente ajustados pelo modelo de Langmuir, o qual apontou que a máxima adsorção de Ni (71.440 mg kg-1) ocorreu após 12 semanas de contato do Ni com amostras do subsolo. A afinidade do Ni também foi maior pelas amostras de subsolo (1,0 L kg-1). A adsorção de Ni foi maior nas amostras superficiais, devido ao menor ponto de efeito salino nulo e ao maior tero de matéria orgânica. A elevação do pH do solo aumentou a adsorção de Ni. Houve menos dessorção de Ni das amostras de solo incubadas por 4 e 12 semanas, sugerindo que as interações entre o Ni e as partículas do solo aumentam ao longo do tempo. A quantidade de Ni dessorvido aumentou com o aumento da força iônica, independentemente da profundidade de amostragem do solo. Finalmente, a histerese da reação de adsorção-dessorção de Ni foi claramente observada. O pH do solo, a força iônica da solução e o tempo de contato do Ni com o solo devem ser considerados critérios para a seleção de áreas para a disposição de resíduos contendo Ni e para compor estratégias de remediação para solos ácricos contaminados por Ni.
ABSTRACT Although nickel (Ni) has both important potential benefits and toxic effects in the environment, its behavior in tropical soils has not been well studied. Nickel adsorption-desorption in topsoil and subsoil samples of an acric Oxisol was studied at three pH values (from 3.0 to 8.0). Adsorption-desorption isotherms were elaborated from experiments with increasing Ni concentration (5 to 100 mg L-1), during 0, 4, and 12 weeks, using CaCl2 0.01 and 0.1 M as electrolytic support in order to also verify the effect of Ni-soil time contact and of ionic strength on the reaction. Experimental results of Ni adsorption fitted Langmuir model, which indicated that maximum Ni adsorption (71,440 mg kg-1) occurred at subsoil, after 12 weeks. Nickel affinity (KL) was also greater at subsoil (1.0 L kg-1). The Ni adsorption in the topsoil samples was higher, due to its lower point of zero salt effect (PZSE) and higher organic matter content. The increase in soil pH resulted in the increase of Ni adsorption. Nickel desorbed less from soil samples incubated for 4 or 12 weeks, suggesting that Ni interactions with colloidal particles increase over time. The amount of Ni desorbed increased with increasing ionic strength in both the topsoil and subsoil soil samples. Finally, adsorption-desorption hysteresis was clearly observed. Soil pH, ionic strength of soil solution and the Ni-soil contact time should be considered as criteria for selecting the areas for disposal of residues containing Ni or to compose remediation strategies for acric soils contaminated with Ni.
https://doi.org/10.1590/1413-70542017411020116
1212 downloads
9.
Influence of Poly-L-Lactic Acid Scaffold's Pore Size on the Proliferation and Differentiation of Dental Pulp Stem Cells
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Conde, Cristian Muniz
; Demarco, Flávio Fernando
; Casagrande, Luciano
; Alcazar, José Carlos
; Nör, Jacques Eduardo
; Tarquinio, Sandra Beatriz Chaves
.
O objetivo desse estudo foi avaliar a influência do tamanho dos poros de um scaffold à base de poli ácido láctico (PLLA) sobre a proliferação e diferenciação de células tronco da polpa dental (dental pulp stem cells - DPSC). Os scaffolds foram preparados dentro da câmara pulpar de discos de terceiros molares (1 mm), utilizando sal como porógeno (150-250 µm ou 251-450 µm). DPSC (1x105 células) foram semeadas nos scaffolds com diferentes tamanhos de poros e cultivadas em placas de 24 poços. A proliferação celular foi avaliada utilizando WST-1 após 3-21 dias. Além disso, RT-PCR foi utilizado para avaliar a diferenciação odontoblástica das DPSC utilizando marcadores da diferenciação odontoblástica (DSPP, DMP-1 e MEPE). RNA obtido de odontoblastos humanos foi utilizado como controle. A taxa de proliferação celular foi semelhante nos dois scaffolds avaliados, exceto no 14° dia, no qual as células cultivadas nos scaffolds com os maiores poros apresentaram uma maior taxa de proliferação (p<0,05). Após 21 dias, as DSPC cultivadas em ambos scaffolds avaliados foram capazes de expressar os marcadores odontoblásticos DMP-1, DSPP e MEPE. Em resumo, ambos scaffolds avaliados nesse estudo permitiram a proliferação e diferenciação odontoblástica das DPSC.
The aim of this study was to evaluate the influence of the poly-L-lactic acid (PLLA)-based scaffold's pore size on the proliferation and differentiation of dental pulp stem cells (DPSCs). The scaffolds were prepared in pulp chambers of 1-mm-thick tooth slices from third molars using salt crystals (150-250 µm or 251-450 µm) as porogen. DPSC (1x105 cells) were seeded in the scaffolds with different pore sizes, and cultured in 24-well plates. The cell proliferation was evaluated using the WST-1 assay after 3-21 days. Furthermore, RT-PCR was used to assess the differentiation of the DPSCs into odontoblasts, using markers of odontoblastic differentiation (DSPP, DSP-1 and MEPE). RNA from human odontoblasts was used as control. Cell proliferation rate was similar in both scaffolds except at the 14th day period, in which the cells seeded in the scaffolds with larger pores showed higher proliferation (p<0.05). After 21 days DPSCs seeded in both evaluated scaffolds were able of expressing odontoblastic markers DMP-1, DSPP and MEPE. In summary, both scaffolds tested in this study allowed the proliferation and differentiation of DPSCs into odontoblast-like cells.
https://doi.org/10.1590/0103-6440201300032
3809 downloads
10.
Characterization of the soil fertility and root system of restinga forests
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Bonilha, Rodolfo Martins
; Casagrande, José Carlos
; Soares, Marcio Roberto
; Reis-Duarte, Rose Mary
.
A Restinga é um conjunto de comunidades vegetais em mosaico, determinadas pelas características de seus substratos resultantes de processos deposicionais e idades. Nesse complexo mosaico encontram-se as fitofisionomias de florestas de restinga em estádio de elevada regeneração (restinga alta) e em estádio de média regeneração (restinga baixa), cada qual com suas características vegetais que as diferenciam. O clima no litoral é do tipo tropical (Köppen). A Restinga, de todos os ecossistemas associados à Mata Atlântica, é o mais frágil e suscetível às perturbações antrópicas. As plantas respondem às características do solo por meio de modificações fisiológicas e morfológicas, de modo a alterar a arquitetura (configuração espacial) de seus sistemas radiculares. Este estudo teve por objetivo caracterizar a fertilidade do solo, por meio dos parâmetros químicos e físicos, sob floresta de restinga alta e baixa, com relação à distribuição do sistema radicular no perfil do solo. Foram estudados quatro locais: (1) Parque Estadual da Ilha Anchieta, município de Ubatuba; (2) Estação Ecológica Jureia-Itatins, Estação Ecológica dos Chauás, município de Iguape; (3) Vila de Pedrinhas, no município de Ilha Comprida; e (4) Parque Estadual da Ilha do Cardoso, município de Cananeia. Os estudos sobre fertilidade do solo foram feitos nas profundidades de 0-5, 0-10, 0-20, 20-40 e 40-60 cm, para as análises químicas e físicas. Também foi avaliada a distribuição do sistema radicular no perfil do solo, utilizando imagens digitais e o programa Spring. Conclui-se que o sistema radicular, para todas as fitofisionomias estudadas, encontra-se nas camadas mais superficiais, 0-10 e 10-20 cm, principalmente na primeira (80 %); que todos os ambientes estudados apresentaram baixa fertilidade do solo, com valores de saturação por bases inferiores a 16 %, em que a maior parte da CTC está ocupada por Al3+; e que a vegetação de restinga é edáfica.
The Restinga vegetation consists of a mosaic of plant communities, which are defined by the characteristics of the substrates, resulting from the type and age of the depositional processes. This mosaic complex of vegetation types comprises restinga forest in advanced (high restinga) and medium regeneration stages (low restinga), each with particular differentiating vegetation characteristics. The climate along the coast is tropical (Köppen). Of all ecosystems of the Atlantic Forest, Restinga is the most fragile and susceptible to anthropic disturbances. Plants respond to soil characteristics with physiological and morphological modifications, resulting in changes in the architecture (spatial configuration) of the root system. The purpose of this study was to characterize the soil fertility of high and low restinga forests, by chemical and physical parameters, and its relation to the root system distribution in the soil profile. Four locations were studied: (1) Ilha Anchieta State Park, Ubatuba; (2) two Ecological Stations of Jureia-Itatins and of Chauás, in the municipality of Iguape; (3) Vila de Pedrinhas in the municipality of Ilha Comprida; and (4) Ilha do Cardoso State Park, Cananeia. The soil fertility (chemical and physical properties) was analyzed in the layers 0-5, 0-10, 0-20, 20-40 and 40-60 cm. In addition, the distribution of the root system in the soil profile was evaluated, using digital images and the Spring program. It was concluded that the root system of all vegetation types studied is restricted to the surface layers, 0-10 and 10-20 cm, but occupies mainly the 0-10 cm layer (70 %); that soil fertility is low in all environments studied, with base saturation values below 16 %, since most exchange sites are occupied by aluminum; and that restinga vegetation is edaphic.
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11.
Nickel adsorption by variable charge soils: effect of pH and ionic strength
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Brazilian Archives of Biology and Technology
- Journal Metrics
The effects of pH and ionic strength (I) on Ni adsorption in variable charge soils were evaluated by laboratory batch experiments. Experimental results fitted the Langmuir model. Maximum adsorption (Ads max) ranged from 260-2818 mg kg-1 (topsoil) to 532-1541 mg kg-1 (subsoil). Nickel affinity (K L) was higher in the subsoil samples (0.022-0.236 L kg-1) than in topsoil (0.003-0.049 L kg-1). Adsorption envelopes showed sharp increase in Ni adsorption (20-90%) in the 4.0-6.0 pH range. Nickel adsorption was affected by I and specific adsorption predominated in the 3.0-5.0 pH range, while above pH 5.0, it was adsorbed by electrostatic mechanisms. Negative values of free energy variation (ΔG) and the separation factor K R<1 indicated that Ni adsorption reaction was favorable and occurred spontaneously, especially when pH increase. Chemical and mineralogical soil attributes should be considered as criteria for selecting the areas for disposal of residues containing Ni to minimize the impact on the environment.
6613 downloads
12.
Adsorção de selênio em latossolos
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Mouta, Ernesto Rinaldi
; Melo, Wanderley José de
; Soares, Marcio Roberto
; Alleoni, Luis Reynaldo Ferracciú
; Casagrande, José Carlos
.
A retenção de Se pelos colóides do solo constitui importante processo para a manutenção da sanidade ambiental. A informação sobre a adsorção de Se em solos altamente intemperizados é restrita e existem poucos padrões quantitativos disponíveis para a definição de estratégias de remediação de áreas contaminadas. Quantidades crescentes de Se (5, 10, 25, 50, 100 e 250 mg L-1), na forma de Na2SeO3, foram adicionadas a amostras de dez Latossolos brasileiros [três Latossolos Vermelho-Amarelos (LVA-1, LVA-2 e LVA-3), dois Latossolos Vermelhos (LV-1 e LV-2), um Latossolo Vermelho eutroférrico (LVef), um Latossolo Vermelho acriférrico (LVwf), dois Latossolos Amarelos (LA-1 e LA-2) e um Latossolo Amarelo acriférrico (LAwf)]. Isotermas de adsorção foram construídas e foi verificado o ajuste dos resultados experimentais aos modelos de Langmuir e de Freundlich. A equação de Langmuir ajustou melhor os resultados de adsorção de Se do que a isoterma de Freundlich. Todas as isotermas apresentaram o formato tipo-L (exponencial), com exceção daquelas obtidas para o LVA-1 e para o LVA-2, que apresentaram comportamento tipo-C (linear). Valores de adsorção máxima (Ads máx), estimada pelo modelo de Langmuir, variaram de 135 (LVA-3) a 2.245 mg kg-1 (LA-1), enquanto os coeficientes de afinidade (K L) estiveram entre 0,002 (LVA-2) e 0,326 (LVA-3). A constante de afinidade estimada pelo modelo de Freundlich (Kf) variou de 13,7 (LVA-2) a 180,1 (LAwf). A adsorção máxima de Se foi mais elevada no LVef e nos Latossolos ácricos (LAwf e LVwf), enquanto os maiores valores de Kf foram encontrados no LV-2, LVef, LVA-3 e LVwf. Não houve correlação entre os atributos dos solos e as constantes de Langmuir. Valores de Kf correlacionaram-se com os teores de argila (r = 0,42*) e com a capacidade de troca de ânions (r = 0,64*).
Selenium (Se) retention by soil colloids is an important process to maintain the environmental quality. Little information is available on Se adsorption in highly weathered tropical soils, and there are few numerical parameters that can be used as references to aid on adoption management strategies in contaminated areas. Increasing amounts of Se (5, 10, 25, 50, 100 and 250 mg L-1), added as Na2SeO3, were equilibrated with samples of ten Brazilian Oxisols [three Typic Hapludoxes (TH-1, TH-2 and TH-3), two Rhodic Eutrudoxes (RE-1 and RE-2), two Xanthic Hapludoxes (XH-1 and XH-2), one Rhodic Hapludox (RH), one Rhodic Acrudox (RA) and one Anionic Acrudox (AA)]. Adsorption isotherms were obtained and the experimental results fitted to Langmuir and Freundlich models. The Langmuir equation fitted better to the experimental data than the Freundlich model. All isotherms had an L-type (exponential) shape, except for TH-1 and TH-2, which had a C-type (linear) shape. Selenium Ads max varied between 135 mg kg-1 (TH-3) and 2.245 mg kg-1 (XH-1) and the affinity constant (K L) varied from 0.002 (TH-2) to 0.326 L kg-1 (TH-3). Affinity constant (Kf) values between 13.7 (TH-2) and 180.1 L kg-1 (AA) were obtained from the Freundlich model. A high Se retention potential was observed on RH and on acric Oxisols (AA and RA), while qualitative parameters indicated RE-2, RH, TH-3 and RA as Oxisols with high Se affinity. No correlations were observed between soil attributes and Langmuir parameters. The Freundlich coefficient (Kf) correlated with clay content (r = 0.42*) and with anion exchange capacity (AEC) (r = 0.64*).
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13.
Efeito do intervalo de dessecação antecedendo a semeadura do milho e do uso de diferentes espécies de plantas de cobertura
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Corrêa, Juliano Corulli
; Hoffmann, Hermann Paulo
; Monquero, Patrícia
; Casagrande, José Carlos
; Puga, Aline Peregrina
.
O intervalo entre a dessecação e a semeadura da cultura de interesse comercial pode favorecer o crescimento e desenvolvimento dessas plantas e, conseqüentemente, aumentar sua produtividade. O objetivo deste trabalho foi avaliar os efeitos de diferentes intervalos de dessecação e uso de diferentes tipos de plantas de cobertura na fertilidade do solo, no teor nutricional e no crescimento inicial da cultura do milho. O experimento foi realizado em condições controladas de casa de vegetação, sendo constituído dos seguintes tratamentos: quatro intervalos de dessecação antecedendo a cultura comercial, que corresponderam a 21, 14, 7 e 0 dias, em interação com três espécies de cobertura vegetal; Crotalaria juncea (crotalária); Pennisetum americanum (milheto) e Brachiaria brizantha cv. marandu (braquiária). O maior intervalo entre a dessecação e a semeadura do milho aumentou o teor de MO, P e K no solo; o teor desses dois nutrientes no solo depende da planta de cobertura em questão. O milho apresentou maior absorção de N, P e K, em razão do maior intervalo de dessecação das plantas de cobertura. O crescimento do milho foi favorecido em razão dos maiores intervalos de dessecação das espécies de cobertura, devendo ser respeitado o intervalo superior a 14 dias para maior disponibilidade de nutrientes às plantas.
The timing of desiccation of the cover crop before crop sowing can favor the development of the plants and, consequently, increase yields. The purpose of this study was to evaluate the effects of intervals after desiccation of distinct cover crops and corn sowing on soil fertility, nutritional content and the initial development of corn. The experiment was carried out under controlled conditions in a greenhouse, and consisted of the following treatments: four desiccation periods preceding the corn crop (21, 14, 7 and 0 days), combined with three cover crop species; Crotalaria juncea (Indian hemp), Pennisetum americanum (pearl millet) and Brachiaria brizantha cv. marandu (brachiaria). The longest time interval preceding corn sowing resulted in higher contents of soil organic matter, phosphorus and potassium; the content of these two nutrients was related to the cover crop species. Longer intervals between desiccation and corn planting resulted in greater absorption of N, P and K by corn plants. Corn development was also favored by longer periods after cover plant desiccation. An interval of more than 14 days should be maintained to ensure greater nutrient availability for the crop.
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14.
Adsorção de boro em solos ácricos em função da variação do pH
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A adsorção de B pelo solo é o principal fenômeno que afeta sua disponibilidade e seu potencial de contaminação. Os objetivos deste estudo foram: (a) investigar os efeitos do pH na adsorção de B em amostras superficiais e subsuperficiais de um Latossolo Vermelho Acriférrico (LVwf) e de um Latossolo Amarelo Ácrico (LAw) - ambos com balanço positivo de cargas no horizonte Bw - e de um Nitossolo Vermelho eutroférrico (NVef); (b) avaliar a adequação do modelo de Langmuir em simular os resultados experimentais de adsorção; e (c) correlacionar os atributos químicos, físicos e mineralógicos dos solos com os valores de adsorção máxima (Ads máx) e do coeficiente de afinidade (K L), derivados das isotermas. Experimentos do tipo "batch" foram realizados para determinação da quantidade de boro adsorvido, tendo como eletrólito-suporte soluções de NaCl 0,01 mol L-1 com 0,1; 0,2; 0,4; 0,8; 1,2; 1,6; 2,0; e 4,0 µg mL-1 de B. Houve aumento da adsorção de B com a elevação do pH e da concentração inicial de B adicionado. Maiores quantidades de B foram adsorvidas na amostra superficial do NVef e nos horizontes Bw positivamente carregados dos Latossolos ácricos. A adsorção de B foi representada por isotermas dos tipos C (linear) e L (exponencial) e adequadamente ajustada pelo modelo de Langmuir. Os parâmetros Ads máx e K L estimados por regressão não-linear não se correlacionaram com o pH. No pH natural, teores de matéria orgânica (MO) e de argila foram as variáveis que mais influenciaram a Ads máx nas camadas superficiais. Nas camadas subsuperficiais, a Ads máx correlacionou-se negativamente com os teores de MO e positivamente com os de gibbsita. Teores de (hidr)óxidos de Fe cristalinos e amorfos estiveram correlacionados aos valores de K L obtidos nas amostras subsuperficiais e ao pH natural, bem como à Ads máx das camadas superficiais após aumento do pH.
Boron (B) adsorption by soils affects its bioavailable contents and contamination potential. The objectives of this study were: (a) to investigate the effects of pH variation on B adsorption by topsoil and subsoil samples from an Anionic "Rhodic" Acrudox (RA), an Anionic "Xanthic" Acrudox (XA) - both with a positive balance of charge in Bw horizon - and a Rhodic Kandiudalf (RK); (b) to evaluate the ability of the Langmuir model of simulating the experimental results of B adsorption; and (c) to correlate chemical, physical and mineralogical soil attributes with the values of maximum adsorption (Ads max) and affinity coefficient (K L), derived from the isotherms. To quantify the amount of adsorbed B, batch experiments were carried out using a 0.01 mol L-1 NaCl solution as a support electrolyte containing 0.1; 0.2; 0.4; 0.8; 1.2; 1.6; 2.0 and 4.0 µg mL-1 of B. An increase of B adsorption was observed after raising the pH (between 3.5 and 8.0) and the initial concentration of added B. Larger amounts of B were adsorbed in topsoil samples from RK and in Bw positively charged horizons from acric Oxisols. Boron adsorption was represented by type-C (linear) and type-L (exponential) isotherms and well fitted by the Langmuir model. Ads max and K L, estimated by nonlinear regressions, were not correlated with the pH. At a natural pH, the organic matter (OM) and clay contents influenced Ads max most in the topsoil samples. In the subsoil layers, Ads max was negatively correlated with OM contents and positively correlated with gibbsite contents. At a natural pH, the contents of free and amorphous Fe (hydr)oxides were correlated with K L values from subsoil samples. After pH increase, the oxide contents were correlated with Ads max values from the topsoil samples.
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15.
Zinc adsorption in highly weathered soils
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O objetivo deste trabalho foi avaliar o efeito do pH e da força iônica sobre a adsorção de zinco, em três solos altamente intemperizados, com predomínio de cargas variáveis. A partir de experimentos tipo " batch" , foram elaboradas isotermas de adsorção, com quantidades crescentes de Zn (0-80 mg L-1), e envelopes de adsorção foram feitos pela reação de amostras de terra com soluções de Ca(NO3)2 0,01, 0,1 e 1 mol L-1 e 5 mg L-1 de Zn, submetidas a variações de pH (3-8). A força direcional da reação de adsorção de Zn foi estimada pela energia livre de Gibbs e pelo fator de separação. As isotermas foram do tipo C, H e L, e os resultados experimentais ajustaram-se ao modelo de Langmuir. A adsorção máxima variou de 59 a 810 mg kg-1, e o coeficiente de afinidade foi maior em subsuperfície (0,13-0,81 L kg-1) do que em superfície (0,01-0,34 L kg-1). A adsorção de Zn foi favorável e espontânea, e mostrou nítido aumento (20-90%) no intervalo de pH entre 4 e 6. Não houve efeito da força iônica nos valores de pH abaixo de 5, o que indica o predomínio de mecanismos de adsorção específica na faixa de pH 3-5. Acima de pH 5 e no subsolo, o Zn foi adsorvido por mecanismos eletrostáticos, já que foi observado efeito da força iônica. Apesar dos efeitos da profundidade e da força iônica, a adsorção de Zn depende principalmente do pH.
The objective of this work was to assess the effects of pH and ionic strength upon zinc adsorption, in three highly weathered variable charge soils. Adsorption isotherms were elaborated from batch adsorption experiments, with increasing Zn concentrations (0-80 mg L-1), and adsorption envelopes were constructed through soil samples reactions with 0.01, 0.1 and 1 mol L-1 Ca(NO3)2 solutions containing 5 mg L-1 of Zn, with an increasing pH value from 3 to 8. Driving force of reaction was quantified by Gibbs free energy and separation factor. Isotherms were C-, H- and L-type and experimental results were fitted to nonlinear Langmuir model. Maximum adsorption ranged from 59-810 mg kg-1, and Zn affinity was greater in subsoil (0.13-0.81 L kg-1) than in the topsoil samples (0.01-0.34 L kg-1). Zinc adsorption was favorable and spontaneous, and showed sharply increase (20-90%) in the 4-6 pH range. No effect of ionic strength was observed at pH values below 5, because specific adsorption mechanisms predominated in the 3-5 pH range. Above pH 5, and in subsoil samples, Zn was adsorbed by electrostatic mechanisms, since ionic strength effect was observed. Despite depth and ionic strength effects, Zn adsorption depends mainly on the pH.
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