1. 中国农业科学院农田灌溉研究所,河南,新乡,453003
2. 中国农业科学院研究生院,北京,100081
3. 塔里木大学水利与建筑工程学院,新疆,阿拉尔,843300
[ "刘栩辰(1997—),男,硕士研究生,主要从事作物生理与水分高效利用研究。E-mail:finaloo@163.com" ]
纸质出版:2023
移动端阅览
刘栩辰, 马守田, 黄超, 等. 黄淮海平原夏玉米需水量和缺水量时空分布特征[J]. 水土保持学报, 2023,37(2):179-186.
LIU Xuchen, MA Shoutian, HUANG Chao, et al. Spatial and Temporal Distribution of Water Requirement and Water Deficiency of Summer Maize in Huang-Huai-Hai Plain[J]. 2023, 37(2): 179-186.
刘栩辰, 马守田, 黄超, 等. 黄淮海平原夏玉米需水量和缺水量时空分布特征[J]. 水土保持学报, 2023,37(2):179-186. DOI: 10.13870/j.cnki.stbcxb.2023.02.021.
LIU Xuchen, MA Shoutian, HUANG Chao, et al. Spatial and Temporal Distribution of Water Requirement and Water Deficiency of Summer Maize in Huang-Huai-Hai Plain[J]. 2023, 37(2): 179-186. DOI: 10.13870/j.cnki.stbcxb.2023.02.021.
为提高黄淮海平原夏玉米的灌溉效率
优化农业资源配置
依据黄淮海平原27个站点70年的试验统计资料
在作物需水量模型、降雨频率分析、作物系数相关理论的基础上
分析不同水文年型夏玉米的需水量和缺水量(即需要补充灌溉的水量)的时空分布。首先
根据各代表点的多年降雨资料
利用皮尔逊—Ⅲ型曲线确定降雨频率分别为25%
50%
75%
95%的4种水文年型及其相应的有效降雨量;其次
利用Penman-Monteith模型计算参考作物需水量
并结合作物系数法估算作物需水量
进而求得在4种水文年型下夏玉米的需水量、缺水量和灌溉需求指数;最后
基于ArcMap 10.7软件对所得到的夏玉米各需水要素进行插值分析
直观地描述黄淮海平原地区夏玉米需水量、缺水量和灌溉需求指数的时空分布特征。结果表明
1951—2020年间
黄淮海平原夏玉米需水量的高值区分布受水文年型变化的影响不大
主要分布在平原中部呈带状分布的区域;缺水量与灌溉需求指数分布特征相似
高值区的范围随干旱程度的升高(水文年型由湿润到干旱)而扩大
且主要分布于平原中部偏北的区域;有效降雨量高值区主要集中在平原东南部
整体分布呈由南至北逐渐递减的趋势。鲁西、冀南、豫北地区夏玉米缺水量高
生产上应以提高水分利用效率为目标;与之相对应的鲁南、苏北和安徽等地
夏玉米对灌溉的依赖低
可以适当地扩大夏玉米种植面积
应以产量为目标。
For improving plain irrigation efficiency of summer maize and optimize the allocation of agricultural resources in the Huang-Huai-Hai
based on the statistical data of 70 a of experiments at 27 plain site
the crop water requirement model
rainfall frequency analysis and crop coefficient
on the basis of relevant theories
the spatial and temporal distribution of water demand and water deficiency (i.e.water needed for supplementary irrigation) of summer corn in different hydrological years were analyzed.Firstly
according to the annual rainfall data of each representative point
four hydrological annual patterns with rainfall frequency of 25%
50%
75%
95% and their corresponding effective rainfall were determined by using the Pearson-Ⅲ curve.Secondly
the Penman-Monteith model was used to calculate the reference crop water requirement
and the crop coefficient approach was used to estimate the crop water requirement
and then the water requirement
water deficiency and irrigation demand indexes of summer maize under the four hydrological year patterns were obtained.Finally
interpolation analysis of each water demand factor of summer maize was carried out based on ArcMap10.7
and spatial and temporal distribution characteristics of water demand
water deficiency and irrigation demand index of summer maize in Huang-Huai-hai Plain were visually described.The results showed that from 1951 to 2020
the distribution of the high value area of summer maize water requirement in Huang-Huai-hai Plain was not affected by the annual variation of hydrological pattern
and mainly distributed in the central region of the plain with a zonal distribution.The distribution characteristics of water deficiency index and irrigation demand index were similar.The range of high value area increased with the increase of drought degree (hydrological year pattern changes from wet to drought)
and mainly distributed in the north of central plain.The high-value area of effective rainfall was mainly concentrated in the southeast of the plain
and the overall distribution showed a decreasing trend from south to north.The water deficiency of summer maize in western Shandong
southern Hebei and northern Henan was high
so the aim of production should be to improve water use efficiency.Correspondingly
in southern Shandong
Northern Jiangsu and Anhui
the dependence of summer maize on irrigation was low
so the planting area of summer maize can be expanded appropriately and the yield should be taken as the target.
国家统计局农村社会经济调查司.中国农业统计资料1949—2019[M].北京:中国统计出版社,2020.
Zhang Y C, Lei H M, Zhao W G, et al. Comparison of the water budget for the typical cropland and pear orchard ecosystems in the North China Plain[J].Agricultural Water Management,2018,198:53-64.
张光辉,费宇红,刘春华,等.华北平原灌溉用水强度与地下水承载力适应性状况[J].农业工程学报,2013,29(1):1-10.
Yin Z J, Xu Y Y, Zhu X Y, et al. Variations of groundwater storage in different basins of China over recent decades[J].Journal of Hydrology,2021,598:e126282.
邵薇薇,黄昊,王建华,等.黄淮海流域水资源现状分析与问题探讨[J].中国水利水电科学研究院学报,2012,10(4):301-309.
Shen H, Leblanc M, Tweed S, et al. Groundwater depletion in the Hai River basin, China, from in situ and GRACE observations[J].Hydrological Sciences Journal,2015,60(4):671-687.
彭致功,刘钰,许迪,等.农业节水措施对地下水涵养的作用及其敏感性分析[J].农业机械学报,2012,43(7):36-41.
Xiang K Y, Li Y, Robert H, et al. Similarity and difference of potential evapotranspiration and reference crop evapotranspiration: A review[J].Agricultural Water Management,2020,232:e106043.
Gong X W, Liu H, Sun J S, et al. Comparison of Shuttleworth-Wallace model and dual crop coefficient method for estimating evapotranspiration of tomato cultivated in a solar greenhouse[J].Agricultural Water Management,2019,217:141-153.
Monteith J I L. Evaporation and environment[J].Symposia of the Society for Experimental Biology,1965,19:205-234.
Penman H L. Natural evaporation from open water, bare soil and grass[J].Proceedings of the Royal Society of London,1948,193(1032):120-145.
王梅,杨倩,郑江华,等.1963—2012年新疆棉花需水量时空分布特征[J].生态学报,2016,36(13):4122-4130.
Qiao S S, Qu Z Y, Gao X Y, et al. Spatial and temporal distribution characteristics of water requirements for maize in Inner Mongolia from 1959 to 2018[J].Water,2020,12(11):e3080.
曹永强,李晓瑞.河北省夏玉米主产区作物需水量和缺水量研究[J].中国农村水利水电,2018(10):141-147.
魏新光,王铁良,李波,等.辽宁省玉米地水分盈亏时空分布特征及灌溉模式分区研究[J].农业工程学报,2018,34(23):119-126.
刘钰,汪林,倪广恒,等.中国主要作物灌溉需水量空间分布特征[J].农业工程学报,2009,25(12):6-12.
刘小刚,符娜,李闯,等.河南省主粮作物需水量变化趋势与成因分析[J].农业机械学报,2015,46(9):188-197.
张力,陈阜,雷永登.黄淮海地区冬小麦—夏玉米生育期内水分供需时空变化特征[J].中国农业大学学报,2020,25(4):1-10.
徐建文,居辉,刘勤,等.黄淮海地区干旱变化特征及其对气候变化的响应[J].生态学报,2014,34(2):460-470.
Cairns J E, Crossa J, Zaidi P H, et al. Identification of drought, heat, and combined drought and heat tolerant donors in maize[J].Crop Science,2013,53(4):1335-1346.
唐晓培,宋妮,陶国通,等.黄淮海地区Hargreaves公式主要参数的空间化处理[J].农业工程学报,2016,32(增刊1):63-70.
George B A, Shende S A, Raghuwanshi N S. Development and testing of an irrigation scheduling model[J].Agricultural Water Management,2000,46(2):121-136.
康绍忠,贺正中,张学.陕西省作物需水量及分区灌溉模式[M].北京:水利水电出版社,1992.
陈玉民,郭国双,王广兴,等.中国主要作物需水量与灌溉[M].北京:水利电力出版社,1995.
Allen R G, Pereira L S, Raes D, et al. Crop evapotranspiration-Guidelines for computing crop water requirements[J].FAO Irrigation and Drainage Paper (FAO),1998,56:1-15.
赵娜娜,刘钰,蔡甲冰.夏玉米作物系数计算与耗水量研究[J].水利学报,2010,41(8):953-959.
Chapagain A K, Orr S. An improved water footprint methodology linking global consumption to local water resources: A case of Spanish tomatoes[J].Journal of Environmental Management,2009,90(2):1219-1228.
邵晓梅,严昌荣.黄河流域主要农作物的降水盈亏格局分析[J].中国农业气象,2007(1):40-44.
靳国栋,刘衍聪,牛文杰.距离加权反比插值法和克里金插值法的比较[J].长春工业大学学报(自然科学版),2003,24(3):53-57.
李德,祁宦,马晓群.安徽省淮北平原夏玉米主要生育时期旱涝指标与影响评估[J].中国农学通报,2013,29(17):208-216.
商蒙非,赵炯超,韩桐,等.1961—2020年中国玉米需水量及水分盈亏的时空变化格局[J].中国农业大学学报,2022,27(4):22-30.
梅茹玉,毛克彪,杜宝裕,等.河北省冬小麦—夏玉米干旱灾害风险评估[J].中国农业资源与区划,2021,43(7):216-231.
张杰,张慧,陈丹丹,等.河南省夏玉米生育期有效降雨量和需水量时空分布特征[J].河南农业科学,2020,49(9):173-180.
南纪琴,肖俊夫,刘战东,等.不同水文年型北方春玉米需水量时空变化特征研究[J].灌溉排水学报,2014,33(增刊1):45-49.
俞建河,吴永林,丁长荣,等.皖东江淮丘陵区不同水文年水稻优化灌溉制度的研究[J].节水灌溉,2017(1):94-97.
康绍忠,史文娟,胡笑涛,等.调亏灌溉对于玉米生理指标及水分利用效率的影响[J].农业工程学报,1998,14(4):82-87.
张雅芳,郭英,沈彦俊,等.华北平原种植结构变化对农业需水的影响[J].中国生态农业学报(中英文),2020,28(1):8-16.
0
浏览量
755
下载量
4
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621