Jiang Jing, Zhai Deng Pan, Zhang Chao Bo
College of Water Resources Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China.
Ying Yong Sheng Tai Xue Bao. 2019 Apr;30(4):1207-1217. doi: 10.13287/j.1001-9332.201904.039.
Agriculture development in arid and semi-arid saline areas is seriously affected by water resources scarcity and excessive fertilization. Understanding the effects of different irrigation and fertilization levels on soil water and salt distribution and silage maize yield would provide scientific basis for determining appropriate irrigation and fertilization amount. The experiment was carried out in a saline field of the Datong Basin in 2015 and 2016. There were three irrigation levels, with the upper limit of soil moisture being controlled at 100% (W), 90% (W) and 80% (W) of the field water capacity. Irrigation amount was calculated based on the average actual water content before irrigation of each treatment. There were four fertilization levels in 2015, 900 kg·hm (F), 750 kg·hm (F), 600 kg·hm(F), and 450 kg·hm(F), and three levels in 2016 (F, F, and F). The total nutrient content of the slow-release compound fertilizer was 48%, with a 30:12:6 ratio of N:PO:KO. Results showed that the surface conductivity of soil increased with the increases of fertilizer application levels. The effects of fertilization on soil salinity in 0-10 cm was significant. Compared with F, the average EC of F in 0-10 cm was decreased by 25.6%-42.7% in 2015 and by 6.4%-7.7% in 2016, respectively. The water content in 20-80 cm decreased with the increases of fertilizer application levels. Compared with F, the average soil water content in 20-80 cm soil layer of F, F, and F increased by 5.9%, 16.7% and 16.7% in 2015, and that of F and F increased by 13.3% and 16.7% in 2016, respectively. The yield of F and F was higher than that of F and F, and W was lower than W and W in both years. There was no significant difference in yield between F and F. Compared with W, decrease in yield of W was less than 15%. Therefore, the application of compound fertilizer 600-750 kg·hm(nitrogen content 180-270 kg·hm), and irrigation levels W and W were suggested to ensure high yield of forage maize in saline soil in this area, without salt accumulation in root zone.
干旱和半干旱盐碱地区的农业发展受到水资源短缺和过度施肥的严重影响。了解不同灌溉和施肥水平对土壤水分、盐分分布及青贮玉米产量的影响,可为确定适宜的灌溉和施肥量提供科学依据。该试验于2015年和2016年在大同盆地的盐碱地进行。设置了三个灌溉水平,土壤水分上限分别控制在田间持水量的100%(W)、90%(W)和80%(W)。灌溉量根据各处理灌溉前的平均实际含水量计算。2015年设置了四个施肥水平,分别为900 kg·hm(F)、750 kg·hm(F)、600 kg·hm(F)和450 kg·hm(F);2016年设置了三个施肥水平(F、F和F)。缓释复合肥总养分含量为48%,氮:磷:钾比例为30:12:6。结果表明,土壤表层电导率随施肥量的增加而升高。施肥对010 cm土层土壤盐分的影响显著。与F相比,2015年F处理010 cm土层平均电导率降低了25.6%42.7%,2016年降低了6.4%7.7%。2080 cm土层含水量随施肥量增加而降低。与F相比,2015年F、F和F处理2080 cm土层平均土壤含水量分别增加了5.9%、16.7%和16.7%;2016年F和F处理分别增加了13.3%和16.7%。两年中,F和F处理的产量均高于F和F处理,W处理产量低于W和W处理。F和F处理产量差异不显著。与W相比,W处理产量降幅小于15%。因此,建议施用600750 kg·hm复合肥(氮含量180270 kg·hm),采用W和W灌溉水平,以确保该地区盐碱地饲用玉米高产,且根区无盐分积累。