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Maize emergence speed and its relationships with water and heat conditions in Northeast China and meteorological assessment of the maize emergence period.

MA Shu-qing1, WANG Qi2, YU Hai3, XU Li-ping3, ZHANG Tie-lin3, JI Ling-ling1**   

  1. (1Meteorological Observatory of Jilin Province, Changchun 130062, China; 2Institute of Meteorological Science of Jilin Province, Changchun 130062, China; 3Agrometeorological Observatory of Jilin Province, Yushu 131106, Jilin, China)
  • Online:2013-08-10 Published:2013-08-10

Abstract: In 2010-2011, a twofactor experiment of water stress and sowing date for spring maize (Zea mays) was conducted to reveal the effects of soil moisture and air temperature on the spring maize emergence speed in Northeast China, and to establish the corresponding models for assessing and predicting the maize emergence period. The maize emergence speed had close relationships with the soil moisture and air temperature. The maize emerged faster under the conditions of more sufficient soil moisture and higher air temperature, while delayed under dry weather and low temperature. Under the conditions of the average soil moisture (S) in 0-20 cm layer being 21%-25%, soil available water capacity (H) being 50-70 mm, and average air temperature (T) being 18-20 ℃, the maize emerged about 10 d after sowing; at the S was 18%-21%, H was 30-50 mm, and T was 16.5-18 ℃, the emergence was prolonged to about 18 d; while at the S was <18%, H was <30 mm, and T was temperature 16.5 ℃, the emergence was prolonged to 25 d, and even, no seedling appeared. The relationships between the interval days from seeding to emergence (D) and the S, H, and T were D=78.017-1.746S-1.642T or D=60.776-0.288H-1.937T. These indicators and models could be applied in the assessment and prediction of the maize emergence period, and in the guidance of drought-resisting activities and weather services.

Key words: growth, population growth., low-concentration CrylAc, cotton leaf roller