盐结皮土壤形成发育过程影响下的能量平衡动态变化

doi:10.12118/j.issn.1000-6060.2023.435

Abstract

Abstract:

Surface energy balance is the crucial link in the interaction between the earth and the atmosphere, and it is essential to study its characteristics with different underlying surfaces to understand heat transfer at the surface. However, limited information is available on the variation characteristics of the energy balance in the formation process of salt-crusted soil. The main difficulty is the limited calculation method for the albedo of the soil surface during the development of salt crust, which remarkably affects the accurate quantitative description of heat transport in saline soil. Therefore, a simulation experiment combined with an energy balance model and an albedo calculation method was applied to quantitatively analyze the characteristics of dynamic variations in the energy balance during the formation and development of salt-crusted soil. The results are as follows: (1) The formation and development process of salt crust on the soil surface could be expressed using the logistic growth model (R²=0.99). (2) Under continuous irradiation (1000 W·m^-2, 16 d), the albedo of the salt-crusted soil was 0.15-0.41 higher than that of the control treatment with continuous development of the salt crust, which decreased the absorbed heat by the soil, consequently reducing the surface temperature of the salt-crusted soil by 16 °C (mean value) compared to the control treatment. (3) The net radiation, sensible-heat flux, latent-heat flux, and soil-heat flux of the salt-crusted soil decreased by 47.9%, 52.4%, 46.8%, and 47.4% (mean value), respectively, compared to that of the control treatment. This reduction happened under the influence of albedo and surface temperature, which further affected the soil profile temperature. The results provided a notable scientific value for further investigation of soil water-heat transport under the influence of the salt crust.

Key words: salt crust, albedo, soil surface temperature, energy balance

WANG Hongchao, LI Xinhu, GUO Min, LI Jialin. Dynamic variation of energy balance under the influence of salt-crusted soil formation and development[J].Arid Land Geography, 2024, 47(3): 424-432.

Figures/Tables 8

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References 42

[1]	Dai S, Shin H, Santamarina J C. Formation and development of salt crusts on soil surfaces[J]. Acta Geotechnica, 2016, 11(5): 1103-1109. doi: 10.1007/s11440-015-0421-9
[2]	Licsandru G, Noiriel C, Duru P, et al. Dissolution-precipitation-driven upward migration of a salt crust[J]. Physical Review E, 2019, 100(3): 032802, doi: 10.1103/PhysRevE.100.032802.
[3]	Wang J Z, Wu J L, Jia H J. Analysis of spatial variation of soil salinization using a hydrochemical and stable isotopic method in a semiarid irrigated basin, Hetao Plain, Inner Mongolia, north China[J]. Environmental Processes, 2016, 3(4): 723-733. doi: 10.1007/s40710-016-0179-6
[4]	Rad M N, Shokri N, Sahimi M. Pore-scale dynamics of salt precipitation in drying porous media[J]. Physical Review E, 2013, 88(3): 032404, doi: 10.1103/PhysRevE.88.032404.
[5]	Nachshon U, Weisbrod N, Dragila M I, et al. Combined evaporation and salt precipitation in homogeneous and heterogeneous porous media[J]. Water Resources Research, 2011, 47(3): W03513, doi: 10.1029/2010WR009677.
[6]	Shimojima E, Yoshioka R, Tamagawa I. Salinization owing to evaporation from bare-soil surfaces and its influences on the evaporation[J]. Journal of Hydrology, 1996, 178(1-4): 109-136. doi: 10.1016/0022-1694(95)02826-9
[7]	Rad M N, Shokri N, Keshmir A, et al. Effects of grain and pore size on salt precipitation during evaporation from porous media[J]. Transport in Porous Media, 2015, 110(2): 281-294. doi: 10.1007/s11242-015-0515-8
[8]	莫治新. 盐结皮对土壤有机质和水分积累的影响[J]. 环境保护科学, 2015, 41(3): 120-121, 138.
	[Mo Zhixin. Effect of salt crust on soil organic and moisture accumulation[J]. Environmental Protection Science, 2015, 41(3): 120-121, 138.]
[9]	Fujimaki H, Shiozawa S, Inoue M. Effect of salty crust on soil albedo[J]. Agricultural and Forest Meteorology, 2003, 118(1-2): 125-135. doi: 10.1016/S0168-1923(03)00110-2
[10]	Wen W, Lai Y M, You Z M. Numerical modeling of water-heat-vapor-salt transport in unsaturated soil under evaporation[J]. International Journal of Heat and Mass Transfer, 2020, 159: 120114, doi: 10.1016/j.ijheatmasstransfer.2020.120114.
[11]	Nachshon U, Shahraeeni E, Or D, et al. Infrared thermography of evaporative fluxes and dynamics of salt deposition on heterogeneous porous surfaces[J]. Water Resources Research, 2011, 47(12): W12519, doi: 10.1029/2011WR010776.
[12]	Li H Y, Fu C B, Guo W D. An integrated evaluation of land surface energy fluxes over China in seven reanalysis/modeling products[J]. Journal of Geophysical Research: Atmospheres, 2017, 122(16): 8543-8566. doi: 10.1002/jgrd.v122.16
[13]	郭浩楠, 汪少勇, 叶虎林, 等. 长江源区典型高寒沼泽草甸地表能量平衡特征及其影响因素[J]. 冰川冻土. [2023-10-16]. http://kns.cnki.net/kcms/detail/62.1072.P.20220920.0945.002.html.
	[Guo Haonan, Wang Shaoyong, Ye Hulin, et al. Characteristics of surface energy budget of typical alpine swamp meadows in the source region Yangtze River and its influencing factors[J]. Journal of Glaciology and Geocryology.
	[ 2023-10-16. http://kns.cnki.net/kcms/detail/62.1072.P.20220920.0945.002.html.]
[14]	曲志瀛. 浅埋地下水位变化对地表能量平衡的影响——以哈头才当为例[D]. 西安: 长安大学, 2021.
	[Qu Zhiying. Influence of shallow groundwater level change on surfaceenergy balance: Taking the example of Hatoucaidang[D]. Xi'an: Chang'an University, 2021.]
[15]	Gran M, Carrera J, Olivella S, et al. Modeling evaporation processes in a saline soil from saturation to oven dry conditions[J]. Hydrolohy and Earth System Sciences, 2011, 15(7): 2077-2089.
[16]	Rodriguez-Navarro C, Doehne E. Salt weathering: Influence of evaporation rate, supersaturation and crystallization pattern[J]. Earth Surface Processes and Landforms, 1999, 24(3): 191-209. doi: 10.1002/(ISSN)1096-9837
[17]	Li X H, Shi F Z. Effects of evolving salt precipitation on the evaporation and temperature of sandy soil with a fixed groundwater table[J]. Vadose Zone Journal, 2021, 20(3): e20122, doi: 10.1002/vzj2.20122.
[18]	唐洋, 李新虎, 郭敏, 等. 不同初始盐分浓度下土壤盐结皮的形成过程及其对蒸发的影响机理[J]. 干旱区地理, 2022, 45(4): 1137-1145.
	[Tang Yang, Li Xinhu, Guo Min, et al. Formation process of soil salt crust and its influence mechanism on evaporation under different initial salt concentrations[J]. Arid Land Geography, 2022, 45(4): 1137-1145.]
[19]	Bittelli M, Campbell G S, Tomei F. Soil physics with Python: Transport in the soil-plant-atmosphere system[M]. Oxford: Oxford University Press, 2015.
[20]	Saito H, Simunek J, Mohanty B P. Numerical analysis of coupled water, vapor, and heat transport in the vadose zone[J]. Vadose Zone Journal, 2006, 5(2): 784-800. doi: 10.2136/vzj2006.0007
[21]	Alkhaler F, Flerchinger G N, Su Z. Shallow groundwater effect on land surface temperture and surface energy balance under bare soil conditions: Modeling and description[J]. Hydrology and Earth System Sciences, 2012, 16(7): 1817-1831. doi: 10.5194/hess-16-1817-2012
[22]	Guo D L, Yang M X, Wang H J. Sensible and latent heat flux response to diurnal variation in soil surface temperature and moisture under different freeze/thaw soil conditions in the seasonal frozen soil region of the central Tibetan Plateau[J]. Environmental Earth Sciences, 2011, 63(1): 97-107. doi: 10.1007/s12665-010-0672-6
[23]	Eloukabi H, Sghaier N, Ben Nasrallah S, et al. Experimental study of the effect of sodium chloride on drying of porous media: The crusty-patchy efflorescence transition[J]. International Journal of Heat and Mass Transfer, 2013, 56(1-2): 80-93. doi: 10.1016/j.ijheatmasstransfer.2012.09.045
[24]	Zhang C M, Li L, Lockington D. Numerical study of evaporation-induced salt accumulation and precipitation in bare saline soils: Mechanism and feedback[J]. Water Resources Research, 2014, 50(10): 8084-8106. doi: 10.1002/wrcr.v50.10
[25]	Shokri-Kuehni S M S, Vetter T, Webb C, et al. New insights into saline water evaporation from porous media: Complex interaction between evaporation rates, precipitation and surface temperature[J]. Geophysical Research Letters, 2017, 44(11): 5504-5510. doi: 10.1002/grl.v44.11
[26]	Bergstad M, Shokri N. Evaporation of NaCl solution from porous media with mixed wettability[J]. Geophysical Research Letters, 2016, 43(9): 4426-4432. doi: 10.1002/grl.v43.9
[27]	王俏懿, 马耀明, 王宾宾, 等. 喜马拉雅南北坡地区地表能量通量及蒸散发量对比分析[J]. 地球科学进展, 2021, 36(8): 810-825. doi: 10.11867/j.issn.1001-8166.2021.065
	[Wang Qiaoyi, Ma Yaoming, Wang Binbin, et al. Comparative analysis of surface energy flux and evapotranspiration over the northern and southern slopes of the Himalayas[J]. Advances in Earth Science, 2021, 36(8): 810-825.] doi: 10.11867/j.issn.1001-8166.2021.065
[28]	Mahdavi S M, Fujimaki H. Soil salinity resistance effect on evaporation[J]. Eurasian Soil Science, 2019, 52(5): 526-534. doi: 10.1134/S1064229319050089
[29]	Bittelli M, Ventura F, Campbell G S, et al. Coupling of heat, water vapor, and liquid water fluxes to compute evaporation in bare soils[J]. Journal of Hydrology, 2008, 362(3-4): 191-205. doi: 10.1016/j.jhydrol.2008.08.014
[30]	Deb S K, Shukla M K, Sharma P, et al. Coupled liquid water, water vapor, and heat transport simulations in an unsaturated zone of a sandy loam field[J]. Soil Science, 2011, 176(8): 387-398. doi: 10.1097/SS.0b013e318221f132
[31]	Fujimaki H, Shimano T, Inoue M, et al. Effect of a salt crust on evaporation from a bare saline soil[J]. Vadose Zone Journal, 2006, 5(4): 1246-1256. doi: 10.2136/vzj2005.0144
[32]	Li X H, Guo M, Wang H C. Impact of soil texture and salt type on salt precipitation and evaporation under different hydraulic conditions[J]. Hydrological Processes, 2022, 36(11): e14763, doi: 10.1002/ hyp.14763.
[33]	郭敏, 李新虎, 王弘超, 等. 盐结皮厚度对土壤水盐分布特征的影响[J]. 干旱区地理, 2023, 46(8): 1303-1313.
	[Guo Min, Li Xinhu, Wang Hongchao, et al. Effect of salt crust thickness on distribution characteristics of soil water and salt[J]. Arid Land Geography, 2023, 46(8): 1303-1313.]
[34]	Radcliffe D E, Simunek J. Soil physics with HYDRUS: Modeling and applications[M]. New York: CRC Press, 2010.
[35]	Kumar N, Arakeri J H. Evaporation from confined porous media due to controlled IR heating from above[J]. Transport in Porous Media, 2018, 125(2): 311-340. doi: 10.1007/s11242-018-1120-4
[36]	Gran M, Carrera J, Massana J, et al. Dynamics of water vapor flux and water separation processes during evaporation from a salty dry soil[J]. Journal of Hydrology, 2011, 396(3-4): 215-220. doi: 10.1016/j.jhydrol.2010.11.011
[37]	Li X H, Shi F Z. Salt precipitation and evaporative flux on sandy soil with saline groundwater under different evaporation demand conditions[J]. Soil Research, 2021, 60(2): 187-196. doi: 10.1071/SR21111
[38]	Li X H, Shi F Z. The effect of flooding on evaporation and the groundwater table for a salt-crusted soil[J]. Water, 2019, 11(5): 1003, doi: 10.3390/w11051003.
[39]	蔡福, 祝青林, 何洪林, 等. 中国月平均地表反照率的估算及其时空分布[J]. 资源科学, 2005, 27(1): 114-120.
	[Cai Fu, Zhu Qinglin, He Honglin, et al. Estimation and spatio-tmporal distribution of monthly mean surface albedo in China[J]. Resources Science, 2005, 27(1): 114-120.]
[40]	Li X H, Guo M. Experimental study of evaporation flux, salt precipitation, and surface temperature on homogeneous and heterogeneous porous media[J]. Advances in Civil Engineering, 2022, 2022: 7434471, doi: 10.1155/2022/7434471.
[41]	Saito M, Yang P, Loeb N G, et al. A novel parameterization of snow albedo based on a two-layer snow model with a mixture of grain habits[J]. Journal of the Atmospheric Sciences, 2019, 76(5): 1419-1436. doi: 10.1175/JAS-D-18-0308.1
[42]	Shokri N, Or D. Drying patterns of porous media containing wettability contrasts[J]. Journal of Colloid and Interface Science, 2013, 391: 135-141. doi: 10.1016/j.jcis.2012.08.074 pmid: 23123032

参数	平方和（SS）	自由度（df）	方差（MS）	F	显著性（P）	相关系数（r）
净辐射（R_n）	781596.51	1	781596.51	205.30	0.00	0.93
感热通量（H_s）	125501.24	1	125501.24	230.80	0.00	0.94
潜热通量（LE）	5448.66	1	5448.66	0.34	0.56	0.11
土壤热通量（G）	207938.64	1	207938.64	58.15	0.00	0.81

Dynamic variation of energy balance under the influence of salt-crusted soil formation and development

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