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首页> 外文期刊>American journal of enology & viticulture >Determination of Evapotranspiration and Crop Coefficients for a Chardonnay Vineyard Located in a Cool Climate
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Determination of Evapotranspiration and Crop Coefficients for a Chardonnay Vineyard Located in a Cool Climate

机译:凉爽气候下霞多丽葡萄园的蒸散量和作物系数的测定

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A study was conducted in a Chardonnay vineyard located in the Carneros district of Napa Valley to derive vineyard evapotranspiration (ET_c) and seasonal crop coefficients (K_c) values. The vineyard was planted on 2.13 m rows, using a vertical shoot-positioned trellis. Vineyard ET_c was measured using the soil water balance method. Soil water content (SWC) was measured in one-fourth of an individual vine's soil profile (six access tubes per site) to a depth of 2.75 m. In addition, vines were irrigated with applied water amounts at 0.25, 0.5, 0.75, 1.0, and 1.25 of estimated vineyard ET_c. Vineyard ET_c the first year of the study was ~400 mm. Thereafter calculated vineyard ET_c (the product of reference ET [ET_o and the K_c) ranged from 346 to 503 mm per season. Midday leaf water potential (Ψ_l), leaf net CO_2 assimilation rate (A), and stomatal conductance (g_s) were used to indirectly validate estimated ET_c (to determine that vines were not stressed for water) and the derived K_c values. Midday Ψ_l, A, and g_s were linearly related with applied water amounts and SWC across irrigation treatments and years. The diurnal measurements of A and g_s resulted in differences among irrigation treatments, from early morning until late afternoon, with significant differences among treatments dependent upon actual applied water amounts. The results from this study are the first in which vineyard ET_c has been measured on vines grown at a cool vineyard site in California. Estimates of ET_c from this study would be valid for a vineyard with a row spacing of 2.13 m and a canopy vertically positioned using a maximum K_c of 0.74.
机译:在位于纳帕谷Carneros区的霞多丽葡萄园进行了一项研究,以得出葡萄园的蒸散量(ET_c)和季节性作物系数(K_c)值。葡萄园用垂直的芽架固定在2.13m的行上。葡萄园ET_c使用土壤水分平衡法进行测量。在每棵葡萄树土壤剖面的四分之一(每个部位六个接入管)中测量土壤水分(SWC),深度为2.75 m。另外,用估计的葡萄园ET_c的0.25、0.5、0.75、1.0和1.25的灌溉水灌溉葡萄藤。研究第一年的葡萄园ET_c为〜400 mm。此后,计算得出的葡萄园ET_c(参考ET [ET_o和K_c的乘积)在每个季节346至503毫米之间。午间叶片水势(Ψ_1),叶片净CO_2同化率(A)和气孔导度(g_s)用于间接验证估计的ET_c(以确定葡萄树的水分压力不大)和得出的K_c值。整个灌溉处理和年份中,day_1,A和g_s与施水量和SWC线性相关。从清晨到下午,A和g_s的昼夜测量结果导致灌溉处理之间存在差异,而处理之间的显着差异则取决于实际应用的水量。这项研究的结果是首次在加利福尼亚的一个凉爽的葡萄园现场对葡萄藤ET_c进行了测量。这项研究对ET_c的估计对于行距为2.13 m且顶篷垂直定位且最大K_c为0.74的葡萄园有效。

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