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首页> 外文期刊>Transactions of the ASABE >EVAPOTRANSPIRATION AND CROP COEFFICIENTS FOR SEEPAGE-IRRIGATED WATERMELON WITH PLASTIC MULCH IN A SUB-TROPICAL REGION
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EVAPOTRANSPIRATION AND CROP COEFFICIENTS FOR SEEPAGE-IRRIGATED WATERMELON WITH PLASTIC MULCH IN A SUB-TROPICAL REGION

机译:亚热带地区渗灌西瓜塑料膜的蒸散和作物系数

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The crop coefficient (K-c) method is the most widely used method for computing crop evapotranspiration (ETc) and relies on selecting a representative K-c value for a specific production system, soil, and climate. Literature-based (e. g., FAO-56) K-c values, used in the absence of local K-c, can lead to erroneous ETc estimates. This error becomes considerably high when the standard K-c values from the open-field production systems are applied to plastic mulch production systems with seepage irrigation that results in shallow water table conditions. A three-year study (2003-2005) was conducted with two large drainage lysimeters (length = 4.87 m, width = 3.65 m, and depth = 1.37 m) to quantify ETc and K-c for seepage-irrigated watermelon under plastic mulch in sub-tropical Florida. The seasonal ETc varied from 344 to 422 mm, with an average of 373 mm. The K-c values for initial, development, mid-season, and late stages were 0.64, 1.00, 1.28, and 1.15, respectively, and were statistically higher than the values reported in the literature, including FAO-56. The initial K-c especially was greater than the literature values due to low plant cover and high surface soil moisture in the row-middle areas at the beginning of the season resulting from frequent rainfall and shallow water table. To adjust K-c for the effect of variable rainfall wetting on evaporation during the initial stage, a multivariate regression model (r(2) = 0.74) was developed as a function of rainfall and solar radiation. Use of literature-based K-c values resulted in underestimation of seepage-irrigated ETc by 26% to 43%; the 26% underestimation was from a comparison using the same lysimeter setup and seasons but with drip (surface) irrigation. Such large differences, not reported earlier, highlight the importance of developing local K-c for a specific irrigation method, climate, and production system. Regression models (r(2) = 0.96) were developed for predicting K-c as functions of time and growing degree days. With approximately 65,000 ha of vegetables grown under seepage irrigation in Florida, there is a need for developing local K-c values for irrigation management and water allocations. Scaling up the errors in water use from literature-based K-c values to Florida's seepage-irrigated vegetable lands for one season per year showed errors of 25 to 42 million m(3) of water. This error accounts for 15% to 25% of annual rainfall and is likely to be much higher for dual cropping systems within a year. The extent of errors and related effects on watershed water balances highlight the need for similar studies for other seepage-irrigated mulched crops
机译:作物系数(K-c)方法是计算作物蒸散量(ETc)的最广泛使用的方法,它依赖于为特定的生产系统,土壤和气候选择代表性的K-c值。在缺乏本地K-c的情况下使用基于文献的(例如FAO-56)K-c值可能会导致ETc估计错误。当将露天生产系统的标准K-c值应用于渗灌的塑料覆盖物生产系统(导致地下水位较低)时,此误差会变得非常高。进行了为期三年的研究(2003年至2005年),使用两个大型排水渗漏测定仪(长= 4.87 m,宽= 3.65 m,深= 1.37 m)对亚膜覆盖下渗灌西瓜的ETc和Kc进行定量。热带佛罗里达。季节性ETc从344毫米到422毫米不等,平均为373毫米。初期,发育期,中期和后期的K-c值分别为0.64、1.00、1.28和1.15,在统计上高于包括FAO-56在内的文献报道的值。最初的K-c特别高于文献值,这是由于季节开始时行降雨频繁和浅水区造成的中低排植物覆盖率低和表层土壤湿度高。为了在初始阶段调整K-c以适应降雨变化对蒸发的影响,建立了多元回归模型(r(2)= 0.74)作为降雨和太阳辐射的函数。使用基于文献的K-c值导致渗灌灌溉的ETc低估了26%至43%; 26%的低估是通过使用相同的溶渗仪设置和季节但使用滴灌(地面)灌溉进行的比较。如此巨大的差异(先前未曾报道过)凸显了开发针对特定灌溉方式,气候和生产系统的当地钾肥的重要性。开发了回归模型(r(2)= 0.96)来预测K-c作为时间和生长日数的函数。在佛罗里达州,大约有65,000公顷的蔬菜通过渗灌进行种植,因此需要为灌溉管理和水分配制定当地的K-c值。从基于文献的K-c值到佛罗里达每年渗水灌溉的菜地,每年用一个季节扩大一次的用水误差,显示出25至4200万立方米(3)的水。该误差占年降雨量的15%至25%,并且对于一年二季种植的系统来说可能更大。错误的程度和对流域水量平衡的相关影响凸显了对其他渗灌水覆盖作物的类似研究的需求

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