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首页> 外文期刊>Agricultural Engineering International: CIGR Ejournal >Soil water storage and its temporal association with other water-atmospheric variables in a tomato field under different irrigation regimes
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Soil water storage and its temporal association with other water-atmospheric variables in a tomato field under different irrigation regimes

机译:不同灌溉方式下番茄田土壤水储量及其与其他水分-大气变量的时间相关性

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摘要

This study was conducted to evaluate the effect of different irrigation regimes on soil water dynamics and temporal associations with other water-atmospheric variables in a tomato field under different drip irrigation regimes in southwestern Nigeria. The experiment was 3 x 3 randomized complete block design (RCBD) with a split plot arrangement of treatments in three replicates. Irrigation frequencies of applying water every 7, 5 and 3 days designated as F1, F2, and F3, respectively serve as the main plot of the experiment while irrigation depth of 100, 75 and 50% of crop water requirement ( ) designated as D1, D2 and D3 are the sub-plots. During the growing season, soil water storage (SWS) was monitored in soil depths of 0-5, 5-10, 10-20 and 20-30 cm using oven dry method while daily rainfall and crop evapotranspiration ( ) were obtained using rain gauge and daily weather data, respectively. Both classical statistics and time series (state-time) analyses were applied to the data of SWS , P (rainfall + irrigation) and ETc. Irrigation water regimes significantly (pF3D2F2D1F3D3D2F2D3F1D1F1D2F1D3. There was high amplitude of temporal variability of soil water storage while the maximum SWS was obtained in all depths at 86 DAP of tomato. There was strong temporal association between SWS and but not with P. Classical regression of from combinations of and gave low values of coefficient of determination ( R 2 ) (not more than 24%) while about 4 times as that value was obtained from state-time analysis. Employing the state-time approach, the effect of irrigation on soil water dynamics and how stored water is related to other variables was clearly recognized. Therefore, the state-time approach can be a specialized statistical tool for evaluating temporal associations among soil properties and processes under different management scenarios.
机译:本研究旨在评估尼日利亚西南部不同滴灌条件下番茄田不同灌溉方式对土壤水分动力学和时间相关性的影响,以及其他水-大气变量之间的关系。实验是3 x 3随机完整块设计(RCBD),采用三份重复处理的分割图布置。分别以F1,F2和F3为间隔的每7、5和3天浇水的灌溉频率为该实验的主要图,而将灌溉深度的100%,75%和50%的作物需水量()命名为D1, D2和D3是子图。在生长季节,使用烘箱干燥法在0-5、5-10、10-20和20-30 cm的土壤深度中监测土壤蓄水量(SWS),而使用雨量计获得每日降雨量和农作物蒸散量()。和每日天气数据。古典统计量和时间序列(状态时间)分析均应用于SWS,P(降雨+灌溉)和ETc的数据。灌溉水位显着(pF3D2> F2D1> F3D3D2F2D3> F1D1> F1D2> F1D3。土壤水储量的时间变化幅度较大,而番茄在86 DAP处的所有深度都获得最大的SWS,SWS之间存在强烈的时间相关性,但没有P.结合使用的经典回归得到的确定系数(R 2)低的值(不超过24%),而从状态时间分析获得的值约为该值的4倍。时间法,灌溉对土壤水动力学的影响以及储水与其他变量之间的关系已得到清晰认识,因此,状态时间法可以作为一种专门的统计工具,用于评估不同管理情景下土壤特性与过程之间的时间关联性。

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