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DRIP IRRIGATION SCHEDULING OF CITRUS ORCHARD IN TUNISIA

机译:突尼斯柑橘园的滴灌时间表

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Drip irrigation scheduling of Clementine mandarin grove (planted since 1978) wasrncarried out at citrus orchard located at Cap Bon on the Mediterranean coast ofrnTunisia, with layered soil (sandy on sandy clay loam). The irrigation schedulingrnprogram was monitored using a simple method based on soil water status among thernprospected rooting zone (soil water balance and potential) coupled with crop waterrnrequirements determination, during three years, from 2005 to 2007.From the obtained results, the following conclusions would be drawn:1. Prospecting showed that Clementine root system was located by 65% in the toprnsoil surface layer and the remaining part is located in the subsequent layer with arnparticular root concentration (25%) within the layer’s transition zone. No rootsrnhave been observed growing deeper than 1.00 m.2. Soil moisture characterization is useful to identify the water retention and tornestablish the frequency of soil watering,rn3. Soil water potential associated to soil moisture measurement represents arnsuitable way to estimate water deficit and irrigation scheduling,rn4. Irrigation triggering should be conducted in two phases. During the “flowering-rnJune physiological fruit drop” period (February - June) the irrigation should berntriggered when the 0.25 m deep tensiometer reading reaches 10 × 10~(-3) MPa (0.1rnbar) while during the period of “fruit growth-ripening” (July-October) the tensionrnwould be 15 × 10~(-3) MPa (0.15 bar). These critical levels of soil water tensionsrncould be recommended in order to establish an irrigation scheduling of citrusrncultivated on low water retention sandy soilsrn5. The following three dimensional regression model could describe the seasonalrnsoil moisture distribution, within the root zone under drip irrigation: Z = 0.054 + 0.873 10~(-3) × - 0.23 10~(-5) x~2 - 0.00163 y + 0.258 10~(-4) y~2 - 0.83 10~(-6) x y(r~2=0.82~(**))The obtained results, has given in hand materials for the dissemination of the testedrnmethodological approach. When used properly, it can enhance the irrigator’s chancesrnof success.
机译:在位于突尼斯地中海沿岸Cap Bon的柑桔园进行了柑桔柑桔滴灌计划(自1978年开始种植),土壤层状(沙质壤土上的沙质)。在2005年至2007年的三年中,采用简单的方法,根据预期生根区之间的土壤水状况(土壤水平衡和潜力)以及确定作物需水量,对灌溉计划进行了监测,从中得出以下结论:绘制:1。勘探表明,柑桔根系位于表层土壤表层的65%处,其余部分位于随后的层中,该层过渡带内的根状根浓度为25%。没有观察到根深超过1.00 m.2的情况。土壤水分表征对于确定水分保持力和确定土壤浇水频率是有用的。与土壤湿度测量相关的土壤水势代表了估算缺水量和灌溉计划的合适方法。灌溉触发应分两个阶段进行。在“开花期-6月生理性果实下降”期间(2月-6月),当0.25 m深的张力计读数达到10×10〜(-3)MPa(0.1rnbar)时,应停止灌溉,而在“果实生长- ”(7月至10月),张力将为15×10〜(-3)MPa(0.15 bar)。可以建议这些临界水平的土壤水分张力,以便建立在低保水性沙质土壤上栽培的柑桔的灌溉计划。以下三维回归模型可以描述滴灌条件下根区内的季节性土壤水分分布:Z = 0.054 + 0.873 10〜(-3)×-0.23 10〜(-5)x〜2-0.00163 y + 0.258 10 〜(-4)y〜2-0.83 10〜(-6)xy(r〜2 = 0.82〜(**))获得的结果已在手边提供了用于传播测试方法的材料。如果使用得当,它可以提高灌溉机的成功率。

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