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首页> 外文期刊>Agricultural Water Management >Seasonal basal crop coefficient pattern of young non-bearing olive trees grown in drainage lysimeters in a temperate sub-humid climate
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Seasonal basal crop coefficient pattern of young non-bearing olive trees grown in drainage lysimeters in a temperate sub-humid climate

机译:温带亚湿润气候排水型液晶仪中生长的幼小非承载橄榄树的时令基础作物系数模式

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Young non-bearing olive trees were grown in drainage lysimeters and their water consumption was measured over two consecutive yearly-experimental periods to analyze the effect ofseasonal variations on the basal crop coefficient (K-cb). Micro-lysimeter measurements were used to quantify soil evaporation (E-s) and E-s was subtracted from evapotranspiration (ETc) to determine transpiration. Monthly mean (K-cb) were determined as (ETc-E-s)/ETo, where ETo is the FAO-PM grass-reference evapotranspiration, calculated from locally measured weather data. The observed K-cb value at mid-season, 0.38, was obtained in the fall months, with 41% of canopy cover. The mid-season K-cb when adjusted to the FAO-56 standard climate was 0.43. Seasonal patterns of K-cb are presented and the K-cb value during the mid-season growth-stage was found to be similar to those described in the literature for Mediterranean climates. Variation of the basal crop coefficient was satisfactorily explained by measured canopy light interception (FIR) and a linear regression model is presented for K-cb as a function of FIR.
机译:年轻的非含橄榄树在排水型溶液中生长,并在连续两个年度实验期间测量它们的用水量,以分析基部作物系数(K-CB)的季期期变化的影响。微尿素测量测量用于量化土壤蒸发(E-S),并从蒸散蒸腾(ETC)中减去E-S以确定蒸腾。每月平均值(K-CB)被确定为(ETC-E-S)/ EtO,其中EtO是FAO-PM基层蒸散,从本地测量的天气数据计算。在秋季的季节中观察到的K-CB值为0.38,在秋季获得,41%的冠层盖。调整到FAO-56标准气候时期的季节K-CB为0.43。呈现K-CB的季节性模式,发现季节生长阶段的K-CB值类似于地中海气候文献中描述的那些。通过测量的冠层光拦截(FIR)令人满意地解释基底作物系数的变化,并且作为冷杉的函数呈现K-CB的线性回归模型。

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