| 覆土浅埋滴灌玉米田双作物系数模型参数全局敏感性分析 |
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| 引用本文： | 戚迎龙,赵举,史海滨,尹春艳,曹国军,李彬,李敏.覆土浅埋滴灌玉米田双作物系数模型参数全局敏感性分析[J].农业工程学报,2020,36(7):99-108. |
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| 作者姓名： | 戚迎龙 赵举 史海滨 尹春艳 曹国军 李彬 李敏 |
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| 作者单位： | 内蒙古农业大学水利与土木建筑工程学院,呼和浩特 010018;内蒙古农牧业科学院资源环境与检测技术研究所,呼和浩特 010031;内蒙古农牧业科学院资源环境与检测技术研究所,呼和浩特 010031;内蒙古农业大学水利与土木建筑工程学院,呼和浩特 010018;吉林农业大学资源与环境学院,长春 130118;内蒙古科技大学包头师范学院,包头 014030 |
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| 基金项目： | 内蒙古农牧业创新基金（2017CXJJN11）；国家自然科学基金重点项目（51539005）；国家重点研发计划（2018YFD0300402、2017YFD0201505）；国家科技支撑计划（2014BAD12B03） |
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| 摘 要： | 为深刻了解双作物系数模型参数对覆土浅埋滴灌玉米田蒸散发耗水结构及水分传输过程的影响,采用拓展傅里叶幅度敏感性检验法对模型参数进行全局敏感性分析,筛选出敏感参数,提高调参校准的效率和精准度。结果表明:参数±10%变化时,全生育期土壤蒸发量、作物蒸腾量、蒸散发耗水量最大值较最小值分别高18.72%、25.37%、19.9%。土壤蒸发是表土水分的消耗过程,总量在最大、最小值条件下1 m土层日贮水量动态接近,而作物蒸腾是消耗整个根系层内土壤水,总量变化对1 m土层水分消耗的影响较大。土壤蒸发总量的敏感参数为土壤表层可蒸发水量、生长中期基础作物系数,其全局敏感性指数为0.662、0.321,是不敏感参数均值的33.6~69.4倍。作物蒸腾总量的敏感参数为根系不受水分胁迫的临界土壤贮水量、生长中期基础作物系数、田间持水量,其敏感性指数为0.569、0.485、0.455,是不敏感参数均值的34.5~43倍。敏感参数与蒸发蒸腾的关系为:表土完全湿润后,其可蒸发水量决定干燥过程土壤蒸发量,二者正相关。中期基础作物系数影响蒸发系数,总蒸发量与其负相关。根系不受水分胁迫的临界土壤贮水量越高,玉米根区易利用的水量区间越窄,根系越早发生水分胁迫,作物蒸腾受限,总蒸腾量与其负相关。中期基础作物系数与总蒸腾量正相关,对其影响程度远高于初期、后期基础作物系数。田间持水量高的土壤能在灌溉、降雨量较大时存贮更多水分用于作物蒸腾,总蒸腾量与其正相关。
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| 关 键 词： | 蒸散发 模型 敏感性分析 双作物系数 覆土浅埋滴灌 玉米 |
| 收稿时间： | 2019/9/8 0:00:00 |
| 修稿时间： | 2020/2/10 0:00:00 |
Global sensitivity analysis of model parameters of dual crop coefficient in subsurface drip irrigated maize field |
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| Qi Yinglong,Zhao Ju,Shi Haibin,Yin Chunyan,Chao Guojun,Li Bin and Li Min.Global sensitivity analysis of model parameters of dual crop coefficient in subsurface drip irrigated maize field[J].Transactions of the Chinese Society of Agricultural Engineering,2020,36(7):99-108. |
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| Authors: | Qi Yinglong Zhao Ju Shi Haibin Yin Chunyan Chao Guojun Li Bin and Li Min |
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| Institution: | 1.Water Conservancy and Civil Engineering College of Inner Mongolia Agricultural University, Hohhot 010018, China; 2.Institute of Resources and Environment and Detection Technology of Inner Mongolia Academy of Agricultural & Animal Husbandry Science, Hohhot 010031, China;,2.Institute of Resources and Environment and Detection Technology of Inner Mongolia Academy of Agricultural & Animal Husbandry Science, Hohhot 010031, China;,1.Water Conservancy and Civil Engineering College of Inner Mongolia Agricultural University, Hohhot 010018, China;,2.Institute of Resources and Environment and Detection Technology of Inner Mongolia Academy of Agricultural & Animal Husbandry Science, Hohhot 010031, China;,3.College of Resources and Environment of Jilin Agricultural University, Changchun, 130118, China ;,2.Institute of Resources and Environment and Detection Technology of Inner Mongolia Academy of Agricultural & Animal Husbandry Science, Hohhot 010031, China; and 4.Baotou Teacher''s College of Inner Mongolia Technology University, Baotou 014030, China |
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| Abstract: | Abstract: The purpose of this research was to study parameters of double crop coefficient model that were sensitive to evapotranspiration of the maize field under shallow buried drip irrigation condition. The global sensitivity analysis of the model parameters was carried out by the extended Fourier amplitude sensitivity test (EFAST) method, and the sensitive parameters were selected to improve the efficiency and precision of the model by adjusting these sensitive parameters. The field experiments were carried out in Institute of Agricultural Science of Tongliao, Inner Mongolia, China (43.74°N, 122.55°E, 164m, elevation above mean sea level) in 2017. The results showed that when the values of model parameters were fluctuated within ±10%, the maximum soil evaporation was 18.72% higher than the minimum value, the maximum crop transpiration was 25.37% higher than the minimum value, and the maximum evapotranspiration was 19.9% higher than the minimum value during the whole growing season of maize. Soil evaporation was a process of the consumption of surface soil water, thus the dynamic difference of daily soil water storage in 1 m soil layer was small. Crop transpiration was a process of the consumption of soil water in the root layer of maize, thus the change of total crop transpiration resulted in a greater impact on the water consumption of 1m soil layer. When the total soil evaporation in the whole growing season of maize was simulated, the sensitive parameters were evaporable water on soil surface and basic crop coefficient of middle growth period, and their corresponding global sensitivity indexes were 0.662 and 0.321, respectively. Their global sensitivity indexes were 33.6-69.4 times higher than the mean of insensitive parameters. When the total crop transpiration during the whole growing season was simulated, the sensitive parameters were the threshold of soil water storage of roots free from water stress, basic crop coefficient of middle growth period and field water capacity, and their corresponding global sensitivity indexes were 0.569, 0.485 and 0.455, respectively. Their global sensitivity indexes were 34.5-43 times higher than the mean of insensitive parameters. The relationship between sensitive parameters and evapotranspiration were investigated and the results showed that after the topsoil was completely wet, the amount of soil water evaporated determined the amount of soil evaporation during the drying process, and total soil evaporation increased due to the increase of evaporable water on soil surface. The basic crop coefficient of middle growth period changed soil evaporation by affecting the soil evaporation coefficient. The total soil evaporation decreased due to the increase of basic crop coefficient of middle growth period. The higher threshold of soil water storage of roots free from water stress would result in the narrower interval of the available soil water in the root zone of maize, thus limiting crop transpiration. The total crop transpiration was inversely related to it. The basic crop coefficient of middle growth period and the total crop transpiration were positively correlated. The effect of basic crop coefficient of middle growth period on the total crop transpiration was much higher than the basic crop coefficient of initial and end period. The soil with high field water capacity could store more water for crop transpiration when irrigation and rainfall were high, and the total crop transpiration increased with the increase of field water capacity. The results provide theoretical support for exploring efficient water management methods of maize cultivation under shallow buried drip irrigation. |
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| Keywords: | evapotranspiration models sensibility analysis dual crop coefficient drip irrigation in shallow buried soil maize |
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