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SIMULATING DEEP PERCOLATION IN FLOOD-IRRIGATED MATURE PECAN ORCHARDS WITH RZWQM2

机译:用RZWQM2模拟深水成熟Pecan果园的深层渗透

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摘要

The timing and amount of irrigation water are critical to the optimum production of pecans in semi-arid, irrigated agriculture systems. However, few tools are available to managers for measuring or estimating water use compared to deep percolation (DP) below the root zone. The RZWQM2 model was compared to the daily water balance method at two flood-irrigated mature pecan orchards, with different soil textures and depths to water table, in the lower Rio Grande Valley near Las Cruces, New Mexico, to characterize: (I) DP below the upper 100 cm soil profile, and (2) the effects of DP on water table levels. At site I (sandy loam) and site 2 (silty clay loam), comparisons between measured and simulated soil water contents at different soil depths during March to December in 2009 and 2010 demonstrated that RZWQM2 generally provided satisfactory predictions of soil water dynamics but consistently undepredicted soil water content after irrigation. Total estimated and simulated DP at site I were 489.1 and 445.2 mm in 2009, and 541.5 and 465.8 mm in 2010, respectively. Thus, at site 1, 25% to 29% of the applied water percolated below the root zone, but the model underpredicted these values by 3 to 4 percentage points. In contrast, total estimated DP at site 2 was 37% and 35% of the total water, and again the model underpredicted by 4 to 5 percentage points. Water table levels at site I were affected by DP following irrigation events. This was likely related to the relatively shallow water table and the highly permeable sandy loam soil in the upper layers. Nevertheless, the root zone water balance at site I did not appear to be influenced by the water table since downward hydraulic fluxes were predominant below 40 cm depth and soil water content remained constant at 160 cm depth. In contrast, the deeper water table at site 2 was not influenced by DP. Calibration and validation of RZWQM2 with field data at pecan orchards with different soil textures and water table depths allow managers to use the model to address water management issues to minimize DP while optimizing pecan production.
机译:灌溉时间和灌溉水量对半干旱,灌溉农业系统中山核桃的最佳生产至关重要。但是,与根部区域下方的深层渗滤(DP)相比,管理者几乎没有可用的工具来测量或估算用水量。在新墨西哥州拉斯克鲁塞斯附近的里奥格兰德河谷下游,在两个洪涝灌溉的成熟山核桃果园中,将RZWQM2模型与每日洪水平衡方法进行了比较,这两个山核桃果园的土壤质地和地下水位不同低于上部100 cm的土壤剖面,以及(2)DP对地下水位的影响。在地点I(沙质壤土)和地点2(粉质壤土),2009年和2010年3月至12月不同土壤深度的实测土壤水分和模拟土壤水分之间的比较表明,RZWQM2通常提供令人满意的土壤水动力学预测,但始终无法预测灌溉后土壤含水量。 I地的估计和模拟总DP值在2009年分别为489.1和445.2毫米,在2010年分别为541.5和465.8毫米。因此,在站点1,25%到29%的应用水渗透到了根区以下,但是该模型将这些值低估了3-4个百分点。相比之下,站点2的总DP估计值占总水量的37%和35%,并且该模型再次低估了4至5个百分点。灌溉事件发生后,地点I的地下水位受到DP的影响。这可能与地下水位相对浅和上层的高渗透性沙壤土有关。不过,由于向下的水力通量主要在40 cm深度以下,而土壤水分在160 cm深度保持恒定,因此I点的根区水平衡似乎不受地下水位的影响。相反,站点2的较深地下水位不受DP的影响。通过使用具有不同土壤质地和地下水位深度的山核桃果园的田间数据对RZWQM2进行校准和验证,管理人员可以使用该模型解决水管理问题,从而在优化山核桃产量的同时最大限度地减少DP。

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