Energy balance of irrigated intercropping field in the middle reaches of Heihe River basin

被引:0
作者
Jinkui Wu
Yongjian Ding
Genxu Wang
Yongping Shen
Yamazaki Yusuke
Kubota Jumpei
机构
[1] Chinese Academy of Sciences,Cold and Arid Regions Environmental and Engineering Research Institute
[2] The Laboratory of Climate Study of China Meteorological Administration,undefined
[3] Research Institute for Humanity and Nature,undefined
来源
Chinese Geographical Science | 2006年 / 16卷
关键词
radiation budget; energy balance; intercropping field; Heihe River basin;
D O I
暂无
中图分类号
学科分类号
摘要
Based on the experiments conducted in an irrigated intercropping field in Zhangye Oasis in the middle reaches of Heihe River basin in 2004, the characteristics of radiation budget are analyzed. Furthermore, energy balance is calculated by using Bowen-Ratio Energy Balance (BREB) method. The results show that the ratio of the absorbed radiation to the incoming short radiation in intercropping crop canopy-soil system is increasing with growing stages, from 0.81 in the initial growing stage (IGS) to 0.86 in the late growing stage (LGS). The net radiation, which is smaller in IGS, increases rapidly in the first period of the middle growing stage (MGS) and reaches the maximum value in the second period of MGS. It then somewhat decreases in LGS. The ratio of net radiation to total radiation has a similar trend with the net radiation. In the whole growing stages, latent heat flux, which takes up 70% or so of the net radiation, is the dominant item in energy balance. Sensible heat flux shares 20% of the net radiation and soil heat flux has a percentage of 10%. The characteristics of heat balance vary distinctly in different growing stages. In IGS, the ratios of latent heat flux, sensible heat flux and soil heat flux to net radiation are 44.5%, 23.8% and 31.7% respectively. In MGS, with the increasing of latent heat flux and the decreasing of sensible heat flux and soil heat flux, the ratios turn into 84.4%, 6.3% and 9.3%. In LGS, the soil heat flux maintains 0W/m2 or so, and latent heat flux and sensible heat flux take up 61.4% and 38.6% respectively. The energy balance also shows an obvious daily variation characteristic.
引用
收藏
页码:243 / 248
页数:5
相关论文
共 28 条
[1]  
Amarakoon D.(2000)Estimating daytime latent heat flux and evapotranspiration in Jamaica Agricultural and Forest Meteorology 102 113-124
[2]  
Chen A.(1999)Evapotranspiration model for semi-arid shrub-lands tested against data from SE Spain Agricultural and Forest Meteorology 95 67-84
[3]  
Mclean P.(1994)Energy balance and latent heat flux partitioning in coffee hedge rows at different stages of canopy development Agricultural and Forest Meteorology 68 173-86
[4]  
Domingo F.(1991)Soil and canopy energy balances of arrow crop at partial cover Agronomy Journal 83 744-753
[5]  
Villagarcia L.(1996)Sensible heat and latent heat transpiration in oasis cropland Arid Land Geography 19 68-74
[6]  
Brenner A. J.(2003)Crop coefficients and water-use estimates for sugarcane based on long-term Bowen ratio energy balance measurements Field Crops Research 83 125-138
[7]  
Gutierrez M. V.(1989)Energy balance and water use of cereal crops Agricultural and Forest Meteorology 48 135-147
[8]  
Meizer C. F.(2004)Effect of water allocation of the Heihe River on plan structure and stable development of the ecosystem in the Linze Oasis, Gansu: A case study in the Pinchuan Irrigation District in Linze County at the middle reaches of the Heihe River Journal of Glaciology and Ggeocryology 26 333-343
[9]  
Ham J. M.(1996)Analysis of land surface evaporation and heat balance in the transitional zone of oasis-desert Arid Land Geography 19 80-87
[10]  
Heilman J. L.(1997)Seasonal variation of energy budget and evapotranspiration partitioning in wheat field Acta Geographica Sinica 52 536-542