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Evaluation of the CropSyst Model during Wheat-Maize Rotations on the North China Plain for Identifying Soil Evaporation Losses

机译:华北平原小麦-玉米轮作过程中CropSyst模型用于识别土壤蒸发损失的评估

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摘要

The North China Plain (NCP) is a major grain production zone that plays a critical role in ensuring China's food supply. Irrigation is commonly used during grain production; however, the high annual water deficit [precipitation (P) minus evapotranspiration (ET)] in typical irrigated cropland does not support double cropping systems (such as maize and wheat) and this has resulted in the steep decline in the water table (~0.8 m year−1 at the Luancheng station) that has taken place since the 1970s. The current study aimed to adapt and check the ability of the CropSyst model (Suite-4) to simulate actual evapotranspiration (ETa), biomass, and grain yield, and to identify major evaporation (E) losses from winter wheat (WW) and summer maize (SM) rotations. Field experiments were conducted at the Luancheng Agro-ecosystem station, NCP, in 2010–2011 to 2012–2013. The CropSyst model was calibrated on wheat/maize (from weekly leaf area/biomass data available for 2012–2013) and validated onto measured ETa, biomass, and grain yield at the experimental station from 2010–2011 to 2011–2012, by using model calibration parameters. The revalidation was performed with the ETa, biomass, grain yield, and simulated ETa partition for 2008–2009 WW [ETa partition was measured by the Micro-lysimeter (MLM) and isotopes approach available for this year]. For the WW crop, E was 30% of total ETa; but from 2010–11 to 2013, the annual average E was ~40% of ETa for the WW and SM rotation. Furthermore, the WW and SM rotation from 2010–2011 to 2012–2013 was divided into three growth periods; (i) pre-sowing irrigation (PSI; sowing at field capacity) to emergence period (EP), (ii) EP to canopy cover period (CC) and (iii) CC to harvesting period (HP), and E from each growth period was ~10, 60, and 30%, respectively. In general, error statistics such as RMSE, Willmott's d, and NRMSE in the model evaluation for wheat ETa (maize ETa) were 38.3 mm, 0.81, and 9.24% (31.74 mm, 0.73, and 11.89%); for wheat biomass (maize biomass) they were 1.25 Mg ha−1, 0.83, and 9.64% (0.78 Mg ha−1, 0.96, and 7.96%); and for wheat grain yield (maize grain yield) they were 0.65 Mg ha−1, 0.82, and 9.87% (0.2 Mg ha−1, 0.99, and 3.79%). The results showed that CropSyst is a valid model that can be use with a reliable degree of accuracy for optimizing WW and SM grain yield production and water requirement on the NCP.
机译:华北平原(NCP)是主要的粮食生产区,在确保中国粮食供应方面发挥着关键作用。谷物生产过程中通常使用灌溉。但是,典型的灌溉耕地每年的高水亏缺[降水量(P)减去蒸散量(ET)]不支持双重种植系统(例如玉米和小麦),这导致地下水位急剧下降(〜0.8)自1970年代以来发生的m年 −1 。当前的研究旨在适应和检验CropSyst模型(Suite-4)模拟实际蒸散量(ETa),生物量和谷物产量的能力,并确定冬小麦(WW)和夏季的主要蒸发量(E)损失玉米(SM)轮作。在2010–2011年至2012–2013年间,在新农合栾城县农业生态系统站进行了田间试验。使用小麦/玉米(从2012-2013年的每周叶面积/生物量数据中)对CropSyst模型进行了校准,并使用模型在2010-2011年至2011-2012年的试验站对测得的ETa,生物量和谷物产量进行了验证。校准参数。使用2008-2009年WW的ETa,生物量,谷物产量和模拟的ETa分区进行了重新验证[ETa分区是通过今年可用的微溶度计(MLM)和同位素方法测量的]。对于WW作物,E为总ETa的30%;但是从2010-11到2013年,WW和SM轮换的年平均E约为ETa的40%。此外,2010年至2011年至2012年至2013年的WW和SM轮换被分为三个增长期。 (i)播前灌溉(PSI;按田间播种)到出苗期(EP),(ii)EP到冠层覆盖期(CC)和(iii)CC到收获期(HP),以及每次生长的E期间分别为〜10%,60%和30%。通常,小麦ETa(玉米ETa)模型评估中的误差统计量(如RMSE,Willmott d和NRMSE)分别为38.3 mm,0.81和9.24%(31.74 mm,0.73和11.89%);小麦生物量(玉米生物量)分别为1.25 Mg ha -1 ,0.83和9.64%(0.78 Mg ha -1 ,0.96和7.96%);小麦籽粒产量(玉米籽粒产量)分别为0.65 Mg ha -1 ,0.82和9.87%(0.2 Mg ha -1 ,0.99和3.79%) 。结果表明,CropSyst是一个有效的模型,可以以可靠的准确度使用它来优化NCP上的WW和SM谷物产量和需水量。

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