Soil Moisture’s Dynamics in Maize Field of Trrace in Loess Plateau
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Soil Moisture’s Dynamics in Maize Field of Trrace in Loess Plateau
Bulletin of Soiland Water ConservationVol. 24, Issue 6, Pages: 1-4(2005)
作者机构:
1. 南京大学城市与资源系,江苏,南京,210093
2. 中国科学院水利部水土保持研究所, 陕西杨凌,712100
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Published:2005
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ZHAO Yaoyang, LIU Wenzhao, PU Lijie. Soil Moisture’s Dynamics in Maize Field of Trrace in Loess Plateau[J]. Bulletin of Soiland Water Conservation, 2005, 24(6): 1-4.
DOI:
ZHAO Yaoyang, LIU Wenzhao, PU Lijie. Soil Moisture’s Dynamics in Maize Field of Trrace in Loess Plateau[J]. Bulletin of Soiland Water Conservation, 2005, 24(6): 1-4.DOI:
Soil Moisture’s Dynamics in Maize Field of Trrace in Loess Plateau
soil moisture dynamics of a maize field was studied. Impacts of different land overs on soil moisture were conducted in comparison with soil moisture of a millet field and fallow field. Theresults showed that precipitation in the raining season played an importantrole in supplying soil water in the maize field and the soil moisture’s dynamic period was coincided with the raining season;different land covers had strong effecton the soil moisture
and the evapotranspiration amounts of maize and millet plots were 502. 9 mm and 473.9 mm
respectively
but the fallow land
only 414.lmm;the ET/ Eo ratio of the maize field (evapotransipration/water surface evaporation) in the entire growing period was 0.77
however
its ratios was greater than 1.00 in thejointing stage and the following stage. The ratio for the whole growing period was 0.69 on the millet field.Abstract:Based on the field experiments
soil moisture dynamics of a maize field was studied. Impacts of differentland covers on soil moisture were conducted in comparison with soil moisture of a millet field and fallow field. The results showed that precipitation in the raining season played an importantrole in supplying soil water in the maizefield and the soil moisture’s dynamic period was coincided with the raining ason;different land covers had strong effecton the soil moisture
and the evapotranspiration amounts of maize and millet plots were 502.9 mm and 473.9 mm
respectively
but the fallow land
only 414.lmm;the ET/ Eo ratio of the maize field (evapotransipration/water surface evaporation) in the entire growing period was 0.77
however
its ratios was greater than 1.00 in the jointing stage and the following stage. The ratio for the whole growing period was 0.69 on the millet field.Based on the field experiments
soil moisture dynamics of a maize field was studied. Impacts of different land covers on soil moisture were conducted in comparison with soil moisture of a millet field and fallow field. The results showed that precipitation in the raining season played an importantrole in supplying soil water in the maize field and the soil moisture’s dynamic period was coincided with the raining season;different land covers had strong effecton the soil moisture
and heevapotranspiration amounts of maize and millet plots were 502. 9 mm and 473.9 mm
respectively
but the fallow land
only 414.lmm;the ET/ Eo ratio of the maize field (evapotransipration/water surface evaporation) in the entire growing period was 0.77
however
its ratios was greater than 1.00 in the jointing stage and the following stage. The ratio for the whole growing period was 0.69 on the millet field.