1999
DOI: 10.1016/s0378-3774(98)00092-4
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Causes of high water losses from irrigated rice fields: field measurements and results from analogue and digital models

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Cited by 14 publications
(10 citation statements)
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“…Therefore, the remaining rate of 1.1 mm day −1 was assumed to be the PERC from the fields through the hardpan layer to the deep groundwater. It was reported that the rate of LSEEP is generally higher than the vertical percolation rate 24, 25. Such a low PERC rate seemed to be small compared with typical values reported for Japanese rice fields, which range from 5 to 30 mm day −1 23.…”
Section: Resultsmentioning
confidence: 77%
“…Therefore, the remaining rate of 1.1 mm day −1 was assumed to be the PERC from the fields through the hardpan layer to the deep groundwater. It was reported that the rate of LSEEP is generally higher than the vertical percolation rate 24, 25. Such a low PERC rate seemed to be small compared with typical values reported for Japanese rice fields, which range from 5 to 30 mm day −1 23.…”
Section: Resultsmentioning
confidence: 77%
“…Essa demanda é reflexo da ocorrência de perdas por escoamento superficial, evaporação, fluxo lateral e percolação de água no solo (Stone, 2005). As perdas por percolação podem ser influenciadas por propriedades físicas do solo, largura e estado de consolidação e de conservação das taipas, preparo do solo e por cargas de pressão, decorrentes da altura da lâmina de irrigação (Borrel et al, 1997;Tuong & Bhuiyan, 1999;Walker, 1999;Bouman & Tuong, 2001;Tabbal et al, 2002;Tuong et al, 2005). A percolação é considerada o principal componente das perdas de água em solos arenosos, ocasionando o aumento da lixiviação de nutrientes (Stone, 2005) e, possivelmente, de agrotóxicos, proporcionando a contaminação de águas subterrâneas, as quais muitas vezes podem servir de fonte potá-vel para o consumo humano.…”
Section: A Tecnologia Clearfieldunclassified
“…Some portion of the applied water that is not consumed in agricultural fields flows to streams/drainage canals or is percolated downwards. The movement of water horizontally into the bunds and then vertically downwards to groundwater through the undisturbed soil column within the bunds is termed lateral percolation [7]. Bhuiyan et al [8] reported that seepage and percolation (S & P) are site-specific and depend on soil texture, water table depth, proximity to drainage outlet, and farmer's field water management status.…”
Section: Introductionmentioning
confidence: 99%