2015
DOI: 10.1016/j.agwat.2015.02.009
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Area determination of solar desalination system for irrigating crops in greenhouses using different quality feed water

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Cited by 16 publications
(18 citation statements)
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“…The minimum (MIN), maximum (MAX), mean (AVG), standard deviation (SD), Skewness (SK), Kurtosis (KU), and coefficient of variation (CV) are shown in Table 2. As Table 2 43 PPT, respectively. With a mean of 28.14 PPT, the value of available TDS F is not valid for either drinking or any other use (e.g.…”
Section: Data Processing and General Performancementioning
confidence: 98%
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“…The minimum (MIN), maximum (MAX), mean (AVG), standard deviation (SD), Skewness (SK), Kurtosis (KU), and coefficient of variation (CV) are shown in Table 2. As Table 2 43 PPT, respectively. With a mean of 28.14 PPT, the value of available TDS F is not valid for either drinking or any other use (e.g.…”
Section: Data Processing and General Performancementioning
confidence: 98%
“…A more complete demonstration of these experimental data is given by [36]. Also, a detailed discussion and analysis of comparative investigation between MD and crop water requirement to determine the required area of the solar still system can be found in [43]. Table 4 shows the results of the statistical performance of the ANN model with different node numbers in the hidden layer and different transfer/activation functions.…”
Section: Data Processing and General Performancementioning
confidence: 99%
“…As seen from this table, the solar still desalinations are a good candidate for supplying water in dry climates. They are simple and inexpensive with the least capital and operational costs and can produce freshwater with high quality while being eco‐friendly. However, they need larger areas for their solar collectors while their production capacity and efficiency are low (ie, their GOR is less than 0.5), because of the heat being wasted through the glass …”
Section: Solar‐driven Desalinationsmentioning
confidence: 99%
“…The rough estimate of crop water requirement (CWR) for a typical greenhouse is 0.012 to 0.016 m 3 /d/m 2 . To calculate it exactly, three computational methods of Penman‐Monteith, Fernandez, and Hargreaves are normally employed to calculate the reference evapotranspiration (ET 0 ). Table summarizes these methods and highlights the key parameters considered by each method. Among these, the Penman‐Monteith method calculates the reference evapotranspiration as a function of climatic factors and geographical location parameters, including longitude, latitude, altitude, solar radiation on the grass surface, soil heat flux, air temperature, mean daily wind speed, and actual vapor pressure.…”
Section: Greenhouse Technologymentioning
confidence: 99%
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