收稿日期: 2022-10-17
修回日期: 2022-11-21
网络出版日期: 2023-09-21
基金资助
国家自然科学基金项目(42277314);天山英才-青年科技拔尖人才项目(2022TSYCCX0008);中国科学院西部青年学者(2020-XBQNXZ-012)
Effect of salt crust thickness on distribution characteristics of soil water and salt
Received date: 2022-10-17
Revised date: 2022-11-21
Online published: 2023-09-21
土壤盐结皮对干旱区土壤演化和生态水文过程具有重要影响,目前的研究对于盐结皮土壤的水盐分布特征涉及较少,并且未考虑盐结皮厚度的影响,导致研究结果存在较大差异。因此,通过室内模拟试验,设置4种初始盐分浓度(0 g·L-1、10 g·L-1、150 g·L-1和250 g·L-1)以获取不同盐结皮厚度(4.5 mm、6.6 mm和7.3 mm),采用部分重复逐步退出的方法对比分析土壤剖面水盐的动态变化。结果表明:(1)对比无盐处理,含盐处理盐结皮越厚,土壤剖面含水量越大,含盐量变化幅度越小。(2)试验结束时,4.5 mm厚度盐结皮土壤含水量分布特征和无盐处理相似,6.6 mm和7.3 mm厚度盐结皮土壤剖面含水量显著大于无盐处理(P<0.05)。(3)试验结束时4.5 mm、6.6 mm和7.3 mm厚度盐结皮土壤剖面最小含盐量相比初始含盐量分别减小了90.5%、46.3%和32.1%。研究结果验证了盐结皮厚度会对土壤水盐分布产生较大影响,因此建议未来对于盐结皮土壤水盐分布特征的相关研究需综合考虑盐结皮厚度的影响。
关键词: 盐结皮厚度; 水盐分布特征; 蒸发锋; HYDRUS-1D模型
郭敏 , 李新虎 , 王弘超 , 李佳琳 . 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 . DOI: 10.12118/j.issn.1000-6060.2022.530
Soil salt crust has an important impact on soil evolution and ecohydrological processes in arid areas. There are few recent studies on water and salt distribution characteristics in salt-crust soils, and the influence of salt-crust thickness is not considered, leading to great differences in research results. Therefore, in this paper, four initial salt concentration treatments (0 g·L−1, 10 g·L−1, 150 g·L−1, and 250 g·L−1) were set to obtain different salt-crust thicknesses (4.5 mm, 6.6 mm, 7.3 mm) through laboratory simulation tests, and the soil-profile dynamics of water and salt were compared and analyzed using a partial repeated stepwise withdrawal method. The results were as follows: (1) Compared with the non-salt treatment, the thicker the salt crust, the larger the soil-profile water content, and the smaller the salt-content variation range. (2) At the end of the experiment, the water content distribution characteristics of the 4.5 mm salt-crust soil were similar to those of the unsalted treatment, and the water contents of the 6.6 mm and 7.3 mm salt-crust soils were significantly higher than that of the unsalted treatment (P<0.05). (3) At the end of the test, the minimum salt contents of the 4.5 mm, 6.6 mm, and 7.3 mm salt-crust soils decreased by 90.5%, 46.3%, and 32.1%, respectively, compared with their initial salt contents. The results confirm that salt-crust thickness has a great influence on the distribution of soil water and salt. Therefore, it is suggested that the influence of salt-crust thickness should be considered comprehensively in future research on distribution characteristics of water and salt.
[1] | Li X, Shi F. 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. |
[2] | Dai S, Shin H, Santamarina J C. Formation and development of salt crusts on soil surfaces[J]. Acta Geotechnica, 2015, 11(5): 1103-1109. |
[3] | 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. |
[4] | 邵明安, 王全九, 黄明斌. 土壤物理学[M]. 北京: 高等教育出版社, 2006: 47-76. |
[4] | [Shao Ming’an, Wang Quanjiu, Huang Mingbin. Soil physics[M]. Beijing: Higher Education Press, 2006: 47-76.] |
[5] | Havlin J L. Soil: Fertility and nutrient management[M]. Calabas: CRC Press, 2020: 251-265. |
[6] | Han F X, Banin A, Triplett G B. Redistribution of heavy metals in arid-zone soils under a wetting-drying cycle soil moisture regime[J]. Soil Science, 2001, 166(1): 18-28. |
[7] | Schaufler G, Kitzler B, Schindlbacher A, et al. Greenhouse gas emissions from European soils under different land use: Effects of soil moisture and temperature[J]. European Journal of Soil Science, 2010, 61(5): 683-696. |
[8] | Zhang X, Ye P, Wu Y, et al. Experimental study on simultaneous heat-water-salt migration of bare soil subjected to evaporation[J]. Journal of Hydrology, 2022, 609: 127710, doi: 10.1016/j.jhydrol.2022.127710. |
[9] | 赵文举, 马宏, 范严伟, 等. 不同覆盖模式下砂壤土水盐运移特征研究[J]. 水土保持学报, 2016, 30(3): 331-336. |
[9] | [Zhao Wenju, Ma Hong, Fan Yanwei, et al. Study on the characteristics of water and salt transport in study loam soil under different mulching models[J]. Journal of Soil and Water Conservation, 2016, 30(3): 331-336.] |
[10] | 邓力群, 陈铭达, 刘兆普, 等. 地面覆盖对盐渍土水热盐运动及作物生长的影响[J]. 土壤通报, 2003, 34(2): 93-97. |
[10] | [Deng Liqun, Chen Mingda, Liu Zhaopu, et al. Effects of different ground covers on soil physical properties and crop growth on saline-alkaline soil[J]. Chinese Journal of Soil Science, 2003, 34(2): 93-97.] |
[11] | 宋日权, 褚贵新, 张瑞喜, 等. 覆砂对土壤入渗﹑蒸发和盐分迁移的影响[J]. 土壤学报, 2012, 49(2): 282-288. |
[11] | [Song Riquan, Chu Guixin, Zhang Ruixi, et al. Effects of sand mulching on soil infiltration, evaporation, and salt distribution[J]. Acta Pedologica Sinica, 2012, 49(2): 282-288.] |
[12] | 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. |
[13] | 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. |
[13] | [Mo Zhixin. Effect of salt crust on soil organic and moisture accumulation[J]. Environmental Protection Science, 2015, 41(3): 120-121.] |
[14] | 莫治新, 韩飞, 马萍, 等. 不同盐结皮覆盖对土壤水分时空动态的影响[J]. 北方园艺, 2017(11): 175-178. |
[14] | [Mo Zhixin, Han Fei, Ma Ping, et al. Effect of salt crust on patio-temporal distribution of soil moisture in different thickness[J]. Northern Horticulture, 2017(11): 175-178.] |
[15] | 王晓静, 徐新文, 雷加强, 等. 咸水滴灌下林带的盐结皮时空分布规律[J]. 干旱区研究, 2006, 23(3): 399-404. |
[15] | [Wang Xiaojing, Xu Xinwen, Lei Jiaqiang, et al. Spatiotemporal distribution of salt crust in a shelter-forest belt under drip-irrigation with salt water[J]. Arid Zone Research, 2006, 23(3): 399-404.] |
[16] | Guglielmini L, Gontcharov A, Aldykiewicz A J, et al. Drying of salt solutions in porous materials: Intermediate-time dynamics and efflorescence[J]. Physics of Fluids, 2008, 20(7): 1389, doi: 10.1063/1.2954037. |
[17] | Dashtian H, Shokri N, Sahimi M. Pore-network model of evaporation-induced salt precipitation in porous media: The effect of correlations and heterogeneity[J]. Advances in Water Resources, 2018, 112: 59-71. |
[18] | Gran M, Carrera J, Olivella S, et al. Modeling evaporation processes in a saline soil from saturation to oven dry conditions[J]. Hydrology and Earth System Sciences, 2011, 15(7): 2077-2089. |
[19] | Konukcu F, Istanbulluoglu A, Kocaman I. Determination of water content in drying soils: Incorporating transition from liquid phase to vapour phase[J]. Australian Journal of Soil Research, 2004, 42: 1-8. |
[20] | Rose D A, Konukcu F, Gowing J W. Effect of watertable depth on evaporation and salt accumulation from saline groundwater[J]. Soil Research, 2005, 43: 565-573. |
[21] | Hernández-López M F, Gironás J, Braud I, et al. Assessment of evaporation and water fluxes in a column of dry saline soil subject to different water table levels[J]. Hydrological Processes, 2014, 28(10): 3655-3669. |
[22] | 张建国, 李红伟, 李雅菲, 等. 土壤盐结皮人工培育及其破损程度对土壤蒸发的影响[J]. 农业工程学报, 2019, 35(13): 138-144. |
[22] | [Zhang Jianguo, Li Hongwei, Li Yafei, et al. Artificial cultivation of soil salt crust and effects of its damage rate on soil evaporation[J]. Transactions of the Chinese Society of Agricultural Engineering, 2019, 35(13): 138-144.] |
[23] | 李胜辉, 李诚志, 付小磊. NaCl与Na2SO4风沙土盐结皮力学特性比较分析[J]. 新疆大学学报(自然科学版), 2022, 39(3): 340-349. |
[23] | [Li Shenghui, Li Chengzhi, Fu Xiaolei. Mechanics characteristics of soil salt crust formed by NaCl and Na2SO4[J]. Journal of Xinjiang University (Natural Science Edition), 2022, 39(3): 340-349.] |
[24] | Eloukabi H, Sghaier N, Nasrallah S B, 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 & Mass Transfer, 2013, 56(1-2): 80-93. |
[25] | 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. |
[25] | [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.] |
[26] | Shokri N, Salvucci G. Evaporation from porous media in the presence of a water table[J]. Vadose Zone Journal, 2011, 10: 1309-1318. |
[27] | 魏建涛, 张建新, 范文波, 等. 犁底层深度对膜下滴灌土壤水盐运移影响的模拟研究[J]. 土壤通报, 2021, 52(4): 845-853. |
[27] | [Wei Jiantao, Zhang Jianxin, Fan Wenbo, et al. Effect of the plough bottom depth on the soil water and salt transport under mulched drip irrigation[J]. Chinese Journal of Soil Science 2021, 52(4): 845-853.] |
[28] | 贾浩, 李宝珠, 李文昊. 基于HYDRUS-1D模型的灌排联合下的水盐运移模拟[J]. 节水灌溉, 2021(1): 27-32. |
[28] | [Jia Hao, Li Baozhu, Li Wenhao. Water and salt transport simulation under irrigation and drainage combination based on HYDRUS-1D model[J]. Water Saving Irrigation, 2021(1): 27-32.] |
[29] | 栗现文, 周金龙, 靳孟贵, 等. 高矿化度土壤水分特征曲线及拟合模型适宜性[J]. 农业工程学报, 2012, 28(13): 135-141. |
[29] | [Li Xianwen, Zhou Jinlong, Jin Menggui, et al. Soil-water characteristic curves of high-TDS and suitability of fitting models[J]. Transactions of the Chinese Society of Agricultural Engineering, 2012, 28(13): 135-141.] |
[30] | 廖海, 栗现文, 陈俊英, 等. 原状盐渍土不同盐分含量对土壤水分特征曲线的影响[J]. 节水灌溉, 2021(1): 7-13. |
[30] | [Liao Hai, Li Xianwen, Chen Junying, et al. Effects of different salt contents of undisturbed saline soil on soil moisture characteristic curves[J]. Water Saving Irrigation, 2021(1): 7-13.] |
[31] | 刘涛涛, 王勇辉, 阿迪拉·阿布力米提. 艾比湖湿地不同厚度盐结皮与土壤物理性质的相互关系及其影响因素[J]. 中山大学学报(自然科学版), 2021, 60(6): 91-101. |
[31] | [Li Taotao, Wang Yonghui, Abrimiti Adila. The relationship between different salt crust thickness and soil physical properties in Ebinur Lake Wetland and its influencing factors[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni (Natural Science Edition), 2021, 60(6): 91-101.] |
[32] | Li X, Shi F. 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. |
[33] | 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): 980-990. |
/
〈 |
|
〉 |