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评估华北平原小麦-玉米轮作期间的CropSyst模型以确定土壤蒸发损失

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

作者信息

Umair Muhammad, Shen Yanjun, Qi Yongqing, Zhang Yucui, Ahmad Ayesha, Pei Hongwei, Liu Meiying

机构信息

Key Laboratory of Agricultural Water Resources and Hebei Key Laboratory of Water-Saving Agriculture, Center for Agricultural Resources Research, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang, China.

International College, University of Chinese Academy of Sciences, Beijing, China.

出版信息

Front Plant Sci. 2017 Sep 29;8:1667. doi: 10.3389/fpls.2017.01667. eCollection 2017.

Abstract

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 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 (ET), 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 ET, 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 ET, biomass, grain yield, and simulated ET partition for 2008-2009 WW [ET partition was measured by the Micro-lysimeter (MLM) and isotopes approach available for this year]. For the WW crop, E was 30% of total ET; but from 2010-11 to 2013, the annual average E was ~40% of ET 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 , and NRMSE in the model evaluation for wheat ET (maize ET) 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, 0.83, and 9.64% (0.78 Mg ha, 0.96, and 7.96%); and for wheat grain yield (maize grain yield) they were 0.65 Mg ha, 0.82, and 9.87% (0.2 Mg ha, 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.

摘要

华北平原是主要的粮食产区,对保障中国的粮食供应起着关键作用。粮食生产过程中普遍采用灌溉方式;然而,典型灌溉农田每年的高水分亏缺量(降水量减去蒸发散量)并不支持复种制度(如玉米和小麦),这导致自20世纪70年代以来地下水位急剧下降(在栾城站约为每年0.8米)。本研究旨在调整并检验CropSyst模型(Suite - 4)模拟实际蒸发散量、生物量和粮食产量的能力,并确定冬小麦和夏玉米轮作中主要的蒸发损失。2010 - 2011年至2012 - 2013年在华北平原栾城农业生态系统试验站进行了田间试验。利用2012 - 2013年的每周叶面积/生物量数据对小麦/玉米进行CropSyst模型校准,并使用模型校准参数对2010 - 2011年至2011 - 2012年试验站实测的蒸发散量、生物量和粮食产量进行验证。利用2008 - 2009年冬小麦的蒸发散量划分(通过微型蒸渗仪和同位素方法测量该年的蒸发散量划分)对蒸发散量、生物量、粮食产量和模拟的蒸发散量划分进行再验证。对于冬小麦作物,蒸发量占总蒸发散量的30%;但从2010 - 11年至2013年,冬小麦和夏玉米轮作的年平均蒸发量约占蒸发散量的40%。此外,2010 - 2011年至2012 - 2013年的冬小麦和夏玉米轮作分为三个生长阶段:(i)播前灌溉(土壤田间持水量时播种)至出苗期,(ii)出苗期至冠层覆盖期,(iii)冠层覆盖期至收获期,各生长阶段的蒸发量分别约为10%、60%和30%。总体而言,在小麦蒸发散量(玉米蒸发散量)模型评估中,均方根误差、威尔莫特指数和归一化均方根误差等误差统计量分别为38.3毫米、0.81和9.24%(31.74毫米、0.73和11.89%);对于小麦生物量(玉米生物量),分别为1.25吨/公顷、0.83和9.64%(0.78吨/公顷、0.96和7.96%);对于小麦粮食产量(玉米粮食产量),分别为0.65吨/公顷、0.82和9.87%(0.2吨/公顷。0.99和3.79%)。结果表明,CropSyst是一个有效的模型,可用于以可靠的精度优化华北平原冬小麦和夏玉米的粮食产量及需水量。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4db4/5627545/cd078a78aaec/fpls-08-01667-g0001.jpg

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