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Zhang Mouhui, Tian Zhengchao. Evaluation of the heat pulse method for determining evaporation of a red soil in southern China[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2022, 38(5): 105-111. DOI: 10.11975/j.issn.1002-6819.2022.05.013
Citation: Zhang Mouhui, Tian Zhengchao. Evaluation of the heat pulse method for determining evaporation of a red soil in southern China[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2022, 38(5): 105-111. DOI: 10.11975/j.issn.1002-6819.2022.05.013

Evaluation of the heat pulse method for determining evaporation of a red soil in southern China

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  • Received Date: September 13, 2021
  • Revised Date: December 31, 2021
  • Published Date: March 14, 2022
  • A heat-pulse and sensible heat balance approach has been used for in-situ monitoring soil evaporation at a fine depth scale. However, the accuracy of the heat pulse sensor depends mainly on the meteorological conditions and soil properties. This technique has been tested for the dryland sandy soils in northern China. This study aims to further evaluate the accuracy of the heat pulse method on the red soils (Ultisols) in southern China. A 30-day field experiment was conducted from October 27thto November 25th, 2020, in order to compare the performance of the heat pulse method and commonly-used micro-lysimeter. A three-needle heat pulse sensor was installed in a bare soil profile located at the Huazhong Agricultural University, Wuhan, China. The soil temperature and thermal properties were then determined by the heat pulse sensors, and then the soil evaporation rate was calculated using the sensible heat balance. A net radiometer was installed to monitor the net radiation dynamics for the correction of the surface (Stage I) evaporation errors. The independent daily evaporation rates were measured by micro-lysimeters, which were made of PVC pipes with 10 cm in diameter and 9 cm in depth. The soil water content and meteorological data were collected to evaluate the red soil evaporation from a local weather station. The results showed that the daily evaporation rate by the heat pulse method was agreed better with the measurement of micro-lysimeter, indicating the maximum deviation of 0.80 mm/d and the minimum deviation of 0.02 mm/d during the study period. The coefficient of determination was found to be 0.52 for the daily evaporation rate between the two approaches. Overall, the daily evaporation rate presented an average bias of 0.04 mm/d and the root mean square error of 0.40 mm/d. The reliable cumulative evaporation was obtained with a coefficient of determination of 0.99, compared with the micro-lysimeter. The 30-day cumulative evaporation values were 24.4 and 19.3 mm on average (7-day measurements were not available due to rainfall) measured by the heat pulse method and micro-lysimeters, respectively. The heat pulse method can be expected to automatically capture the fine-scale evaporation dynamics. The heat pulse method can also perform the time-intensive (Sub-hourly) evaporation measurements, rather than the daily measurement in the labor-intensive micro-lysimeter. There was a downward migration of the dry surface layer in the heat pulse method, which was undetectable for the commonly-used lysimeter. Consequently, the daily evaporation rate was the most affected by the soil water content, followed by the net radiation, the wind speed, and the air temperature, according to the soil water content and meteorological records. Anyway, the heat pulse method can reliably determine the evaporation rate of red soil in southern China.
  • [1]
    Or D, Lehmann P, Shahraeeni E, Shokri N. Advances in soil evaporation physics: A review[J]. Vadose Zone Journal, 2013, 12(4): 1-16.
    [2]
    孟春雷. 土壤蒸发及水热传输研究综述[J]. 土壤通报,2007(2):374-378.Meng Chunlei. A review of soil evaporation and moisture and heat transport[J]. Chinese Journal of Soil Science, 2007(2): 374-378. (in Chinese with English abstract)
    [3]
    孟春雷,石建辉. 土壤蒸发研究及对旱灾防治的意义[J]. 防灾科技学院学报,2007(1):83-84.Meng Chunlei, Shi Jianhui. Soil evaporation research and its significance on drought prevention and cure[J]. Journal of Institute of Disaster-Prevention Science and Technology, 2007(1): 83-84. (in Chinese with English abstract)
    [4]
    米美霞. 利用热脉冲方法研究覆盖对土壤蒸发的影响[D]. 杨凌:西北农林科技大学,2013.Mi Meixia. Research on the Effects of Soil Surface Mulch on Soil Evaporation Using Heat Pulse Method[D]. Northwest A&F University, 2013. (in Chinese with English abstract)
    [5]
    汪增涛,孙西欢,郭向红,等. 土壤蒸发研究进展[J]. 山西水利,2007(1):76-78.Wang Zengtao, Sun Xihuan, Guo Xianghong, et al. Advances in soil evaporation research[J]. Shanxi Water Resources, 2007(1): 76-78. (in Chinese with English abstract)
    [6]
    高晓飞,史海珍,杨洁,等. 使用微型蒸发器测定土壤蒸发的研究进展[J]. 水利水电科技进展,2010,30(1):85-90.Gao Xiaofei, Shi Haizhen, Yang Jie, et al. Advances in soil evaporation measured by micro-lysimeter[J]. Advances in Science and Technology of Water Resources, 2010, 30(1): 85-90. (in Chinese with English abstract)
    [7]
    孙宏勇,刘昌明,张永强,等. 微型蒸发器测定土面蒸发的试验研究[J]. 水利学报,2004(8):114-118.Sun Hongyong, Liu Changming, Zhang Yongqiang, et al. Study on soil evaporation by using micro-lysimeter[J]. Journal of Hydraulic Engineering, 2004(8): 114-118. (in Chinese with English abstract)
    [8]
    刘萌,王善举,樊军,等. 利用环刀法快速原位测定土壤蒸发量[J]. 土壤通报,2021,52(1):55-61.Liu Meng, Wang Shanju, Fan Jun, et al. Rapid in-situ determination of soil evaporation with cutting ring method[J]. Chinese Journal of Soil Science, 2021, 52(1): 55-61. (in Chinese with English abstract)
    [9]
    米美霞,樊军,邵明安. 利用热脉冲技术研究石子覆盖对土壤内部蒸发的影响[J]. 土壤学报,2013,50(1):75-82.Mi Meixia, Fan Jun, Shao Mingan. Study of effects of gravel mulch on soil evaporation using heat pulse technology[J]. Acta Pedologica Sinica, 2013, 50(1): 75-82. (in Chinese with English abstract)
    [10]
    Heitman J L, Horton R, Sauer T J, et al. Sensible Heat observations reveal soil-water evaporation dynamics[J]. Journal of Hydrometeorology, 2008, 9(1): 165-171.
    [11]
    Kojima Y, Kawashima T, Noborio K, et al. A dual-probe heat pulse-based sensor that simultaneously determines soil thermal properties, soil water content and soil water matric potential[J]. Computers and Electronics in Agriculture, 2021, 188: 106331.
    [12]
    Heitman J L, Xiao X, Horton R, et al. Sensible heat measurements indicating depth and magnitude of subsurface soil water evaporation[J]. Water Resources Research, 2008, 44(4): 1-7.
    [13]
    Zhang X, Sen L, Heitman J L, et al. Measuring subsurface soil-water evaporation with an improved heat-pulse probe[J]. Soil Science Society of America Journal, 2012, 76(3): 876-879.
    [14]
    张晓. 感热平衡原理测定土壤水分蒸发的改进及分解农田蒸散的实验研究[D]. 北京:中国农业大学,2014.Zhang Xiao. Improvement of Sensible Heat Balance Theory for Determining Soil Water Evaporation and Partitioning Field Evapotranspiration[D]. Beijing: China Agricultural University, 2014. (in Chinese with English abstract)
    [15]
    Xiao X, Heitman J L, Sauer T J, et al. Sensible heat balance measurements of soil water evaporation beneath a maize canopy[J]. Soil Science Society of America Journal, 2014, 78(2): 361-368.
    [16]
    Wang Y Y, Horton R, Xue X Z, et al. Partitioning evapotranspiration by measuring soil water evaporation with heat-pulse sensors and plant transpiration with sap flow gauges[J]. Agricultural Water Management, 2021, 252: 1-8.
    [17]
    Tian Z C, Kool D, Ren T S, et al. Determining in-situ unsaturated soil hydraulic conductivity at a fine depth scale with heat pulse and water potential sensors[J]. Journal of Hydrology, 2018, 564: 802-810.
    [18]
    Xiao X, Horton R, Sauer T J, et al. Cumulative soil water evaporation as a function of depth and time[J]. Vadose Zone Journal, 2011, 10(3): 1016-1022.
    [19]
    Heitman J L, Zhang X, Xiao X, et al. Advances in heat-pulse methods: measuring soil water evaporation with sensible heat balance[J]. Soil Science Society of America Journal, 2020, 84(5): 1371-1375.
    [20]
    Sakai M, Jones S B, Tuller M. Numerical evaluation of subsurface soil water evaporation derived from sensible heat balance[J]. Water Resources Research, 2011, 47(2): 1-17.
    [21]
    Wang Y Y, Ochsner T, Heitman J, et al. Weighing lysimeter data confirm the accuracy and precision of the heat-pulse technique for measuring daily soil evaporation[J]. Soil Science Society of America Journal, 2017, 81(5): 1074-1078.
    [22]
    王晓燕,陈洪松,王克林. 红壤坡地不同土地利用方式土壤蒸发和植被蒸腾规律研究[J]. 农业工程学报,2007,23(12):41-45.Wang Xiaoyan, Chen Hongsong, Wang Kelin. Rules of soil evaporation and plant transpiration under different land use patterns in the sloping land of red soil[J]. Transactions of the Chinese Society of Agricultural Engineering(Transactions of CSAE), 2007, 23(12): 41-45. (in Chinese with English abstract)
    [23]
    姚贤良. 红壤水问题及其管理[J]. 土壤学报,1996(1):13-20.Yao Xianliang. Water problems of red soil and its management[J]. Acta Pedologica Sinica, 1996(1): 13-20. (in Chinese with English abstract)
    [24]
    李王成,王为,冯绍元,等. 不同类型微型蒸发器测定土壤蒸发的田间试验研究[J]. 农业工程学报,2007,23(10):6-13.Li Wangcheng, Wang Wei, Feng Shaoyuan, et al. Field experimental study on the measurement of soil evaporation using different types of micro-lysimeters[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of CSAE), 2007, 23(10): 6-13. (in Chinese with English abstract)
    [25]
    Ren T S, Noborio K, Horton R. Measuring soil water content, electrical conductivity, and thermal properties with a thermo-time domain reflectometry probe[J]. Soil Science Society of America Journal, 1999, 63(3): 450-457.
    [26]
    Kluitenberg G J, Bristow K L, Das B S. Error analysis of heat pulse method for measuring soil heat capacity, diffusivity, and conductivity[J]. Soil Science Society of America Journal, 1995, 59(3): 719-726.
    [27]
    Ochsner T E, Sauer T J, Horton R. Soil heat storage measurements in energy balance studies[J]. Agronomy Journal, 2007, 99(1): 311-319.
    [28]
    Campbell G S, Norman J M. An Introduction to Environmental Biophysics[M]. New York: Springer, 1998.
    [29]
    Tian Z C, Lu Y L, Ren T S, et al. Improved thermo-time domain reflectometry method for continuous in-situ determination of soil bulk density[J]. Soil & Tillage Research, 2018, 178: 118-129.
    [30]
    彭慈德,常留成. 不同温度下红黏土胀缩性试验研究[J]. 长江科学院院报,2019,36(7):100-105.Peng Cide, Chang Liucheng. Experimental study on swelling and shrinkage properties of red clay at different temperatures[J]. Journal of Yangtze River Scientific Research Institute, 2019, 36(7): 100-105. (in Chinese with English abstract)
    [31]
    马稚桐,王文科,赵明,等. 半干旱地区地表-地下水系统水热运移与裸土蒸发研究[J]. 水文地质工程地质,2021,48(4):7-14.Ma Zhitong, Wang Wenke, Zhao Ming, et al. Hydrothermal transfer and bare soil evaporation in surface-groundwatersystems in semi-arid areas[J]. Hydrogeology & Engineering Geology, 2021, 48(4): 7-14. (in Chinese with English abstract)
    [32]
    吴友杰,杜太生. 西北干旱区农田土壤蒸发量及影响因子分析[J]. 农业工程学报,2020,36(12):110-116.Wu Youjie, Du Taisheng. Evaporation and its influencing factors in farmland soil in the arid region of Northwest China[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of CSAE), 2020, 36(12): 110-116. (in Chinese with English abstract)
    [33]
    张静,王力,韩雪,等. 黄土塬区农田蒸散的变化特征及主控因素[J]. 土壤学报,2016,53(6):1421-1432.Zhang Jing, Wang Li, Han Xue, et al. Evapotranspiration of farmland on loess tableland and its major influencing factors[J]. Acta Pedologica Sinica, 2016, 53(6): 1421-1432. (in Chinese with English abstract)

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