Relationship between dry matter accumulation of spring wheat and the water and thermal condition in high altitude area
View Fulltext  View/Add Comment  Download reader
  
DOI:10.7606/j.issn.1000-7601.2013.01.10
Key Words: high altitude area  dryland spring wheat  dry matter accumulation  water and temperature coupling
Author NameAffiliation
MA Xingxiang Institute of Arid Meteorology, CMA/Key Laboratory of Arid Climate Change and Reducing Disaster of Gansu Province/Key Open Laboratory of Arid Climate Change and Disaster Reduction of CMA, Lanzhou, Gansu 730020, China
Wuwei Agricultural Meteorology Experimentation Station of Gansu Province, Wuwe i, Gansu 733000, China 
CHEN Lei  
WANG Helin Institute of Arid Meteorology, CMA/Key Laboratory of Arid Climate Change and Reducing Disaster of Gansu Province/Key Open Laboratory of Arid Climate Change and Disaster Reduction of CMA, Lanzhou, Gansu 730020, China
Wuwei Agricultural Meteorology Experimentation Station of Gansu Province, Wuwe i, Gansu 733000, China 
DING Wenkui Wuwei Agricultural Meteorology Experimentation Station of Gansu Province, Wuwe i, Gansu 733000, China 
YANG Fulin Institute of Arid Meteorology, CMA/Key Laboratory of Arid Climate Change and Reducing Disaster of Gansu Province/Key Open Laboratory of Arid Climate Change and Disaster Reduction of CMA, Lanzhou, Gansu 730020, China
Wuwei Agricultural Meteorology Experimentation Station of Gansu Province, Wuwe i, Gansu 733000, China 
Hits: 264
Download times: 191
Abstract:
      In order to explore the response measures of crop planting under the background of climate changes, the staging seeding test was c onducted to evaluate the influence of water and thermal condition on dry matter accumulation of spring wheat in high altitude area. The result showed that the d ry matter accumulation of spring wheat was positively related with both accumula ted temperature and precipitation at very significant level. If the accumulated temperature increased 50℃·d, the accumulated growth quantity increased 0.2 g· plant-1·d-1; and if the precipitation increased 10 mm, the accumula ted growth quan tity increased 0.11 g·plant-1·d-1 during the dry matter accumulati on period. The coupling index of water and temperature under different seeding stages in two te st years was calculated, and it was found that when the index was high the dry m atter accumulation tended to increase, otherwise it tended to reduce. In the fac tors of water and temperature, the contribution of precipitation was more promin ent to the dry matter accumulation of spring wheat in dryland. There was a very significant positive correlation between the final dry matter accumulation and t he yield. The planting countermeasures were proposed according to the features o f dry matter accumulation and different climate conditions.