摘要
玉米是吉林省西部的主要农作物,水是玉米生产的主要制约因素。如何有效利用有限的水资源,保证玉米高产是亟需解决的问题。通过大田试验,探讨不同播种时间对吉林省西部玉米生产过程中绿水消耗量及其来源的影响,以提高雨水的利用率。3a大田试验的研究结果表明,无论是降水较充足的2005年,还是一般干旱的2006年和极端干旱的2007年,玉米生产需水量中均以绿水消耗量为主,占98%以上。玉米生产的绿水足迹中,2005年以有效降水足迹为主,2006年、2007年以土壤水足迹为主。前3个播期的玉米绿水足迹中有效降水量所占比例,2005年分别为80.4%、87.6%和89.1%,2006年分别为41.3%、43.3%和46.6%,2007年分别为34.2%、35.5%和36.5%。适当晚播使玉米生长季中有相对较多的降水量,气温亦较高,雨热匹配较好,利于玉米生长,而且绿水足迹中有效降水量所占比重也较大。因此,适当晚播有利于提高雨养农业区雨水的利用率,保护土壤水平衡,促进农业的可持续发展。
Maize is the main crop in western Jilin Province. Water is a major constraint on maize production. How to effectively utilize the limited water resources to ensure maize production needs to be solved urgently. Formerly the irrigation water was as the key indicator to measure the water consumption during crop production. However, it neglected the consumption of soil water and water pollution. Water footprint connects the physical and virtual forms of water, which covers blue water, green water and gray water. It can truly reflect water demand and its sources. Recently, the most studies regarding water footprint are to investigate the water footprints of consumer products and products trade between regions or countries. Whereas researching the water footprint in the production process is little. According to the field experiments of maize, we explore the impact of different sowing dates on the source and consumption of green water, to determine the satisfactory degree of precipitation on maize growth and achieve the optimum matching relationship between sowing date and precipitation and temperature in maize growing season under the background of global warming. Results of 3-years experiments showed that either in the rainy year of 2005, or in the drought year of 2006 and extreme drought year of 2007, the green water consumption was the main water requirement in the maize production, which took the ratio over 98%. The green water footprint of maize production was mainly the effective precipitation in 2005 and soil water in 2006 and 2007. Effective precipitation in the green water footprint of the first threesowing dates accounted for 80.4%, 87.6% and 89.1% during 2005, 41.3%, 43.3% and 46.6% during 2006, and 34. 2%, 35.5% and 36.5% during 2007, respectively. It implied that late sowing could gain more precipitation and higher temperature in maize growing stages. Water and thermal resources matched well, which was beneficial to maize production. Moreover, the effective precipitation took large ratio in the green water footprint. Therefore, late sowing is useful to enhance the rate of rainwater utilization, keep the soil water balance and promote the agricultural sustainable development. In the current studies of virtual water and water footprint, the basically method was statistics calculation and analysis. However the statistics do not reflect the differences within the region, the practical production and the water consumption. Field experiments, from the microscopic view, can break through the limitations that the studies of virtual water, water footprint are only from the view of macro- and meso-scale. This paper investigates the regularity of the green water footprint of maize in different sowing dates under the same conditions of soil and cropland management, and provides the basis for the further subdivision of green water and the improvement of green water utilization.
出处
《生态学报》
CAS
CSCD
北大核心
2012年第23期7375-7382,共8页
Acta Ecologica Sinica
基金
国家重点基础研究发展计划(973)项目(2005CB121101)
吉林省科技发展计划项目(20070559)
教育部人文社会科学规划基金项目(10YJA840032)
吉林省教育厅社会科学项目(2007552)
关键词
绿水足迹
不同播种时间
玉米
吉林省西部
green water footprint
different sowing dates
maize
western Jilin province
