| 盐碱土裸土蒸发Ritchie模型修正及验证 |
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| 引用本文： | 郑鑫,李波,衣淑娟.盐碱土裸土蒸发Ritchie模型修正及验证[J].农业工程学报,2016,32(23):131-136. |
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| 作者姓名： | 郑鑫 李波 衣淑娟 |
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| 作者单位： | 黑龙江八一农垦大学工程学院,大庆,163319 |
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| 基金项目： | 黑龙江省自然科学基金资助项目（E201330）；黑龙江八一农垦大学学成、引进人才科研启动计划项目（XDB2013-44） |
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| 摘 要： | 为研究大庆盐碱土区域裸土场地的蒸发规律,并探究Ritchie模型在大庆盐碱土区域的适用性,该文采用微型蒸渗仪对大庆高新区玉米种植场地裸土的蒸发情况进行试验研究,建立相对湿度、降雨量与裸土蒸发量的关系。利用实测值对不同月份Ritchie模型参数进行反算,验证计算所得参数的正确性。结果表明,修正后Ritchie模型计算的蒸发量均方根误差由修正前的3.04 mm/d减少到1.44 mm/d,表明修正模型能够有效地提高盐碱土区域蒸发量计算精度。研究可为黑龙江盐碱土棵间蒸发估算提供参考。
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| 关 键 词： | 土壤 模型 蒸发 盐碱土 裸土 模型修正 |
| 收稿时间： | 6/3/2016 12:00:00 AM |
| 修稿时间： | 2016/10/10 0:00:00 |
Modification and validation of Ritchie model for evaporation of bare saline alkali soil |
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| Zheng Xin,Li Bo and Yi Shujuan.Modification and validation of Ritchie model for evaporation of bare saline alkali soil[J].Transactions of the Chinese Society of Agricultural Engineering,2016,32(23):131-136. |
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| Authors: | Zheng Xin Li Bo and Yi Shujuan |
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| Institution: | College of Engineering, Heilongjiang Bayi Agricultural University, Daqing 163319, China,College of Engineering, Heilongjiang Bayi Agricultural University, Daqing 163319, China and College of Engineering, Heilongjiang Bayi Agricultural University, Daqing 163319, China |
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| Abstract: | Abstract: Ritchie model is popular for evaporation estimation, but it needs to be modified before use in local regions, especially in saline alkaline soil. This study carried out a field experiment to modify the coefficient of Ritchie model. The experiment was carried out in bare field of Daqing City in August and September of 2015. The city had annual precipitation of 427.5 mm and annual evaporation of 1635 mm. The soil was sandy loam. A micro-lysimeter was used for evaporation measurement in bare soil. The lysimeter was 2 mm in thickness, 150 mm in height, and 74 mm in inner diameter. The soil in the lysimeter was replaced every 7 days, and after raining. The effects of rainfall and relative humidity on evaporation were analyzed since the other factors such as temperature and wind speed was similar for the 2 months in the study. The results showed that the relationship between evaporation and relative humidity in these 2 months was similar. The maximum relative humidity was 61% and 43% in August and September, and the mean evaporation was 5.2 and 6.2 mm/d in August and September, respectively. For using Ritchie model, the evaporation limit of the first stage was designed as 8 mm. Using the coefficient value from literature 4.62 mm/d0.5, the model yielded a relatively low evaporation estimation (R2=0.61). Randomly selecting data on 18th-19th in August and on 1st-7th in September, the model coefficient was determined as 2.81 and 0.01 mm/d0.5 for August and September, respectively. Validation using the other data showed that the measured and calculated evaporation values based on the revised coefficient were closely linearly correlated with R2 0.94. The root mean square error was decreased from 3.04 to 0.44 mm/d. Validation using measured evaporation values from maize field in 2016 showed that the measured and calculated values based on revised coefficient were linearly correlated with R2 0.95. Thus, the revised coefficient showed high reliability for evaporation estimation in the study area. |
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| Keywords: | soils models evaporation saline alkali soil bare soil model modification |
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