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首页> 外文期刊>Applied Engineering in Agriculture >COTTON IRRIGATION TIMING WITH VARIABLE SEASONAL IRRIGATION CAPACITIES IN THE TEXAS SOUTH PLAINS
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COTTON IRRIGATION TIMING WITH VARIABLE SEASONAL IRRIGATION CAPACITIES IN THE TEXAS SOUTH PLAINS

机译:德克萨斯南部平原具有可变季节灌溉能力的棉花灌溉时序

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摘要

Within the Ogallala Aquifer Region of Texas, the irrigation capacity (IC) for a given field often changes within a growing season due to seasonal depletion of the aquifer, in-season changes in crop irrigation needs in dry years, or consequences of irrigation volume limits imposed by irrigation district rules. Irrigation planning is further complicated by erratic seasonal rainfall. A field experiment was conducted from 2010 to 2013 to determine cotton (Gossypium hirsutum L.) irrigation productivity using a range of ICs common to the Texas South Plains during three irrigation periods. The treatments included in-season ICs (maximums of 0, 3.2, and 6.4 mm d(-1)) in combination with irrigation periods determined by accumulated growing degree days (GDD(15.6)) and were designated as period 1 (P1 = emergence to 525 GDD(15.6)), period 2 (P2 = 525 to 750 GDD(15.6)), and period 3 (P3>750 GDD(15.6)). Combinations of these factor levels resulted in 27 irrigation treatments with applications made by the low energy precision application (LEPA) method. Annual rainfall totals ranged from 137 to 557 mm over the four years. In all years, results indicated that attempting to store water in the soil profile, or irrigating in excess of the cotton evapotranspiration rate, early in the growing season reduced seasonal irrigation water use efficiency (SIWUE), and sometimes yield, compared to treatments with limited or no early irrigations. Treatments with 0 and 3.2 mm d(-1) ICs during PI used up to 20% less seasonal irrigation with minor yield loss (<2%) compared to treatments with ICs of 3.2 and 6.4 mm d(-1), respectively. This was attributed to water losses caused by evaporation in the region (high wind, low humidity, and high temperatures) from May through June as well as excessive early season vegetative growth resulting in elevated crop transpiration later in the season that could not be met with available IC. Cotton irrigation during the period beyond accumulative cotton GDD(15.6) = 750 was critical for acceptable irrigated yield and high SIWUE. These results provide information to optimize cotton water use in an area with declining irrigation capacity, an advective climate, and increasing pumping restrictions.
机译:在德克萨斯州的奥加拉拉含水层地区,由于含水层的季节性枯竭,干旱年份作物灌溉需求的季节变化或灌溉量限制的结果,给定田地的灌溉能力(IC)通常在生长季节内发生变化。由灌溉区规则强加。季节性降雨不稳定,使灌溉计划更加复杂。从2010年到2013年进行了田间试验,以确定棉花(Gossypium hirsutum L.)的灌溉生产力,使用了德克萨斯州南部平原在三个灌溉期间使用的一系列IC。这些处理包括季节内IC(最大值为0、3.2和6.4 mm d(-1)),并结合由累积生长日数(GDD(15.6))确定的灌溉期,并指定为周期1(P1 =出苗)至525 GDD(15.6)),时段2(P2 = 525至750 GDD(15.6))和时段3(P3> 750 GDD(15.6))。这些因子水平的组合导致了27种灌溉处理方法,这些方法均采用了低能耗精确应用(LEPA)方法。在这四年中,年降雨量总计在137至557毫米之间。在所有年份中,结果表明,与有限的处理相比,在生长期初期尝试在土壤剖面中存储水或灌溉超过棉花的蒸散速率,会降低季节性灌溉用水效率(SIWUE),有时还会降低产量。或没有早期灌溉。与使用3.2和6.4 mm d(-1)的IC处理相比,在PI期间使用0和3.2 mm d(-1)IC的处理分别减少了多达20%的季节性灌溉,且单产损失较小(<2%)。这归因于5月至6月该地区的蒸发(高风,低湿度和高温)造成的水分流失,以及早期营养生长过度,导致该季节后期作物蒸腾增加,而这是无法解决的。可用的IC。对于可接受的灌溉产量和较高的SIWUE,棉花累积GDD(15.6)= 750以外的时期的棉花灌溉至关重要。这些结果为在灌溉能力下降,对流气候和抽水限制增加的地区优化棉花用水提供了信息。

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