Ag?ncias financiadoras: Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gico (CNPq) - Universal 14/2011?482815/2001?6, Universal 28/2018?408393/2018-1; Funda??o de Amparo ? Pesquisa do Estado de Minas Gerais (FAPEMIG) - Demanda Universal Edital 001/2018 Processo CRA-APQ-00597-18 e Demanda Universal Edital 001/2022 Processo CRA-APQ-00458-22; Funda??o de Amparo ? Pesquisa do Estado de S?o Paulo (FAPESP) - FAPESP 2010/51637-0 e BEPE/FAPESP 2012/00676-1. Submitted by Jos? Henrique Henrique (jose.neves@ufvjm.edu.br) on 2022-12-22T23:42:32Z No. of bitstreams: 2 license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) rafaella_loryane_alves_cardoso_landim.pdf: 1618140 bytes, checksum: ff9907e0d0c2f8052e2733090175df88 (MD5) Approved for entry into archive by Jos? Henrique Henrique (jose.neves@ufvjm.edu.br) on 2022-12-23T19:38:22Z (GMT) No. of bitstreams: 2 license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) rafaella_loryane_alves_cardoso_landim.pdf: 1618140 bytes, checksum: ff9907e0d0c2f8052e2733090175df88 (MD5) Made available in DSpace on 2022-12-23T19:38:22Z (GMT). No. of bitstreams: 2 license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) rafaella_loryane_alves_cardoso_landim.pdf: 1618140 bytes, checksum: ff9907e0d0c2f8052e2733090175df88 (MD5) Previous issue date: 2022 Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gico (CNPq) Funda??o de Amparo ? Pesquisa do Estado de Minas Gerais (FAPEMIG) Funda??o de Amparo ? Pesquisa do Estado de S?o Paulo (FAPESP) As veredas e turfeiras s?o ecossistemas especiais para estudos relacionados com a din?mica da mat?ria org?nica. Esses ecossistemas se enquadram no conceito de ?reas ?midas, internacionalmente conhecidas pelo termo ingl?s wetlands, e s?o de alta relev?ncia ambiental para o Cerrado brasileiro. Como s?o originadas da lenta decomposi??o de restos vegetais em ambientes saturados (hidrom?rficos), formam sequ?ncias de solos org?nicos (Organossolos), estocando tanto carbono org?nico quanto ?gua. Al?m da import?ncia h?drica, servem como arquivos cronol?gicos de mudan?as paleoclim?ticas e da evolu??o das paisagens, bem como contribuem para o sequestro de carbono e constituem uma grande biodiversidade. O principal constituinte da mat?ria org?nica desses solos s?o as subst?ncias h?micas (SH), constitu?das por ?cidos h?micos (AH), ?cidos f?lvicos (AF) e humina (HU). O AH ? considerado uma das fra??es mais est?veis e respons?vel pela fixa??o de carbono org?nico no solo e, portanto, sua caracteriza??o ? essencial para entender a sustenta??o dos diferentes ecossistemas. Apesar de existir estudos sobre diferen?as estruturais das fra??es h?micas em diferentes ambientes, o conhecimento deste importante compartimento da mat?ria org?nica, bem como o estudo de t?cnicas espectrosc?picas e qu?micas dos AH extra?dos dos solos de veredas e turfeiras ? praticamente inexistente. Sendo assim, o objetivo deste trabalho foi avaliar a funcionalidade qu?mica dos AH atrav?s da caracteriza??o qu?mica e espectrosc?pica de solos org?nicos de uma turfeira e de uma vereda, respectivamente, da turfeira S?o Jo?o da Chapada (SJC), localizada em Diamantina-MG, e da vereda Parque Nacional de Bras?lia (PNB), localizada em Bras?lia-DF, bem como estabelecer rela??es das caracter?sticas determinadas. Foram estudados testemunhos, ou seja, perfis de solos profundos, coletados com o aux?lio de um vibrotestemunhador. A extra??o e purifica??o dos AH das amostras de solo e o fracionamento qu?mico foram realizadas de acordo com o m?todo recomendado pela Sociedade Internacional das Subst?ncias H?micas com algumas modifica??es, e posteriormente realizado as caracteriza??es qu?micas e espectrosc?picas: acidez total, carbox?lica e fen?lica; espectroscopia na regi?o do ultravioleta-vis?vel (rela??o E4/E6 e ?ndice de fluoresc?ncia) e de infravermelho. Como as ?reas de estudos se situam em regi?es que se diferenciam principalmente quanto aos aspectos de clima, vegeta??o e altitude, existem diferen?as com rela??o ?s caracter?sticas avaliadas. Os resultados obtidos demonstraram que AH extra?dos dos Organossolos da vereda e turfeira apresentam diferen?as em rela??o ? sua composi??o qu?mica e ?s an?lises espectrosc?picas. A fra??o humina predomina nos dois perfis estudados, que ? a fra??o das SH mais resistente ? decomposi??o, seguidos da fra??o de ?cido h?mico e ?cido f?lvico. Em rela??o ao grau de humifica??o, os dois ambientes apresentam alto grau de humifica??o, e de modo geral, as amostras superficiais s?o menos humificadas, enquanto que as mais profundas apresentam maior grau de humifica??o, por apresentarem idades bastante avan?adas. Apresentam tamb?m altos valores de acidez total e fen?lica, e baixa estabilidade estrutural. Tanto a turfeira como a vereda come?aram a se formar durante o Pleistoceno Tardio, portanto, ambos os ambientes sofreram in?meras mudan?as ao longo da evolu??o do solo e da paisagem. Disserta??o (Mestrado) ? Programa de P?s-Gradua??o em Produ??o Vegetal, Universidade Federal dos Vales do Jequitinhonha e Mucuri, 2022. The palm swamp (veredas) and peatlands are special ecosystems for studies related to the dynamics of organic matter. These ecosystems fit into the concept of wetlands, internationally known by the english term wetlands, and are of high environmental relevance for the Brazilian Cerrado. As they originate from the slow decomposition of plant remains in saturated (hydromorphic) environments, they form sequences of organic soils (Histosols), storing both organic carbon and water. In addition to their water importance, they serve as chronological archives of paleoclimatic changes and the evolution of landscapes, as well as contribute to carbon sequestration and constitute a great biodiversity. The main constituent of organic matter in these soils are humic substances (SH), made up of humic acids (AH), fulvic acids (AF) and humin (HU). HA is considered one of the most stable fractions and is responsible for fixing organic carbon in the soil and, therefore, its characterization is essential to understand the sustainability of different ecosystems. Although there are studies on structural differences of humic fractions in different environments, knowledge of this important compartment of organic matter, as well as the study of spectroscopic and chemical techniques of HA extracted from soils of veredas and peatlands is practically non-existent. Therefore, the objective of this work was to evaluate the chemical functionality of HA through the chemical and spectroscopic characterization of organic soils from a peatland and a vereda, respectively, from the S?o Jo?o da Chapada (SJC), located in Diamantina-MG, and from the Brasilia National Park (PNB), located in Bras?lia-DF, as well as establishing relations of the determined characteristics. Cores were studied, that is, profiles of deep soils, collected with the aid of a vibrocore. The extraction and purification of HA from the soil samples and the chemical fractionation were carried out according to the method recommended by the International Society of Humic Substances with some modifications, and afterwards the chemical and spectroscopic characterizations were carried out: total, carboxylic and phenolic acidity; ultraviolet-visible (E4/E6 ratio and fluorescence index) and infrared spectroscopy. As the study areas are located in regions that differ mainly in terms of climate, vegetation and altitude, there are differences in terms of the characteristics evaluated. The results obtained showed that HA extracted from the Histosols of the vereda and peatland present differences in relation to their chemical composition and spectroscopic analyses. The humin fraction predominates in the two profiles studied, which is the fraction of HS most resistant to decomposition, followed by the fraction of humic acid and fulvic acid. Regarding the degree of humification, the two environments present a high degree of humification, and in general, the superficial samples are less humidified, while the deeper samples have a higher degree of humification, due to their very advanced ages. They also present high values of total and phenolic acidity and low structural stability. Both the peatland and the vereda began to form during the late Pleistocene, so both environments underwent numerous changes over the course of soil and landscape evolution.