1997
DOI: 10.2480/agrmet.53.29
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Comparisons of Solar Radiation Interception, Albedo and Net Radiation as Influenced by Row Orientatoins of Crops.

Abstract: Field experiments were conducted on soybean (Glycin max L.) in summer and potato (Solanum tuberosum L.) in autumn to evaluate the effect of row orientations of crops on some selected micrometeorological factors during 1994 and 1995.

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Cited by 12 publications
(14 citation statements)
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“…There was variation in Rn mainly due to differences in surface conditions and row orientations (Baten and Kon, 1997). Latent heat flux accounted for a large portion of Rn as was expected from the sufficient soil water content.…”
Section: Daytime Energy Balance Relationshipsmentioning
confidence: 89%
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“…There was variation in Rn mainly due to differences in surface conditions and row orientations (Baten and Kon, 1997). Latent heat flux accounted for a large portion of Rn as was expected from the sufficient soil water content.…”
Section: Daytime Energy Balance Relationshipsmentioning
confidence: 89%
“…It has been observed recently that row orientations affect solar radiation interception at row canopy, transmission through the canopy, net radiation above and below the canopy and albedo (Baten and Kon, 1997) Ham et al (1991) conducted an experiment on soil and canopy energy balances of row crop at partial cover and examined soil and canopy energy balance separately using Bowen ratio technique. Ham et al (1991), however, considered only N-S row direction in the study, not E-W direction.…”
Section: Introductionmentioning
confidence: 99%
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“…At low solar elevation angles on 35 o 46″ N latitude, penetration of solar radiation is larger at the soil surface between N-S rows that of E-W rows (Baten and Kon, 1997).…”
Section: Introductionmentioning
confidence: 99%
“…The yield of maize may be increased by regulating the soil temperature and interception of solar radiation through the suitable row orientation. Solar radiation interception, penetration and albedo were affected by row orientations (Baten and Kon, 1997). Lower albedo was found at smaller solar zenith (noon hours) or higher sun elevation because of the trapping of reflected radiation beneath the canopy (Millar, 1959;Graham and King, 1961).…”
Section: Introductionmentioning
confidence: 99%