UM NOVO MÉTODO PARA ESTUDOS DINÂMICOS, IN SITU, DA INFILTRAÇÃO DA ÁGUA NA REGIÃO NÃO- SATURADA DO SOLO

A agricultura e a atividade humana que mais afeta o meio ambiente. Imensas quantidades de insumos agricolas sao aplicados sobre o solo e grande parte destes degrada os recursos hidricos. Para uma investigacao adequada do efeito destes insumos, estudam-se as propriedades hidraulicas do solo, que influem no transporte de solutos neste meio. Medir tais propriedades e modelar os parâmetros correlatos sao tarefas extremamente complexas, devido ao tempo requerido, dinheiro, instrumentacao e escala. As metodologias convencionais inferem as propriedades hidraulicas em amostras que estao em equilibrio, atraves de tecnicas invasivas e sob restricoes especiais. esta tes contribui com a Ciencia do Ambiente, via Ciencia do Solo, propondo um novo metodo de estudo da infiltracao da agua na regiao nao-saturada do solo, utilizando a tomografia computadorizada (TC). O tomografo foi aqui desenvolvido e construido. A TC, neste trabalho, mediu a umidade durante o fluxo nao-saturado e, atraves da solucao numerica da equacao de Richards e do modelo Rossi-Nimmo, obtiveram-se a curva de retencao, a sortividade, e a difusividade. Resultados qualitativos, como imagens 2D e 3D, e resultados quantitativos demonstraram a boa correlacao do metodo proposto com o metodo tradicional de medida da curva de retencao. Amostras de solo estruturado foram analisadas em laboratorio e em camp.

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