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یاوری, مرتضی, واعظی, علی رضا, عسکری, محمد صادق. (1404). بررسی نقش ویژگی‏های فیزیکی خاک بر شاخص‌های نفوذ آب در خاک (مطالعه موردی: استان زنجان). سامانه مدیریت نشریات علمی, (), 421-436. doi: 10.22092/ijsr.2026.370662.796
مرتضی یاوری; علی رضا واعظی; محمد صادق عسکری. "بررسی نقش ویژگی‏های فیزیکی خاک بر شاخص‌های نفوذ آب در خاک (مطالعه موردی: استان زنجان)". سامانه مدیریت نشریات علمی, , , 1404, 421-436. doi: 10.22092/ijsr.2026.370662.796
یاوری, مرتضی, واعظی, علی رضا, عسکری, محمد صادق. (1404). 'بررسی نقش ویژگی‏های فیزیکی خاک بر شاخص‌های نفوذ آب در خاک (مطالعه موردی: استان زنجان)', سامانه مدیریت نشریات علمی, (), pp. 421-436. doi: 10.22092/ijsr.2026.370662.796
یاوری, مرتضی, واعظی, علی رضا, عسکری, محمد صادق. بررسی نقش ویژگی‏های فیزیکی خاک بر شاخص‌های نفوذ آب در خاک (مطالعه موردی: استان زنجان). سامانه مدیریت نشریات علمی, 1404; (): 421-436. doi: 10.22092/ijsr.2026.370662.796

بررسی نقش ویژگی‏های فیزیکی خاک بر شاخص‌های نفوذ آب در خاک (مطالعه موردی: استان زنجان)

پژوهش های خاک
مقالات آماده انتشار، پذیرفته شده، انتشار آنلاین از تاریخ 25 اسفند 1404    اصل مقاله (1.24 M)
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.22092/ijsr.2026.370662.796
نویسندگان
مرتضی یاوری؛ علی رضا واعظی* ؛ محمد صادق عسکری
گروه علوم و مهندسی خاک، دانشکده کشاورزی، دانشگاه زنجان، زنجان، ایران.
چکیده
هدف این پژوهش بررسی نقش برخی ویژگی‌های فیزیکی خاک در نفوذ آب به خاک در برخی خاک‌های منطقه نیمه‌خشک زنجان بود. بدین منظور، ۶۸ نقطه با تنوع بافت، کاربری و پوشش گیاهی، انتخاب و آزمایش‌های نفوذ با استفاده از استوانه مضاعف انجام شد. در نمونه‌های خاک (صفر تا 60 سانتیمتر) ۱2 ویژگی فیزیکی اندازه‌گیری شد. شش شاخص نفوذ شامل: نفوذ تجمعی (CI)، نفوذ اولیه (II)، شدت‌ نفوذ اولیه (IIR)، شدت نفوذ نهایی (FIR)، شدت نفوذ متوسط (MIR) و عمق مؤثر نفوذ (EDI) تعیین شدند. نتایج همبستگی پیرسون نشان داد که میانگین وزنی (MWDwet) و هندسی (GMDwet) قطر خاکدانه‌ها در حالت تر با همه شاخص‏های نفوذ رابطه معنی‏دار داشت (p< 0.05). چگالی ظاهری (BD) با CI، II، FIR و  MIR همبستگی معنی‏دار داشت (p< 0.05). نتایج رگرسیونی نشان داد ویژگی‌های فیزیکی خاک شامل: چگالی ظاهری، رطوبت اولیه، سنگریزه، توزیع اندازه ذرات و میانگین هندسی قطر خاکدانه‏ها نقش محوری در تعیین­ نفوذ آب در خاک داشتند. برای انجام تحلیل واریانس یک‌طرفه، خاک­ها در چهار گروه بر مبنای BD، MWDwet و  GMDwet تقسیم شدند. تفاوت معنی­داری بین سطوح مختلف GMDwet از نظر CI، II و FIR وجود داشت (p< 0.05). همچنین تفاوت بین سطوح مختلف MWDwet از نظر CI و II معنی‌دار بود و در مورد سطوح مختلف BD، تفاوت­ها تنها از نظر CI معنی‌دار بود. این پژوهش نشان داد که علاوه بر ساختمان خاک، توزیع اندازه ذرات اولیه نیز با اثرگذاری بر شاخص‌هایی مانند چگالی ظاهری، تخلخل و پایداری خاکدانه‌ها، نقش مؤثری در نفوذ آب در خاک‌های منطقه نیمه‌خشک دارد.
کلیدواژه‌ها
پایداری خاکدانه؛ توزیع اندازه ذرات؛ چگالی ظاهری؛ خاکدانه‌های پایدار در آب؛ میانگین وزنی قطر
عنوان مقاله [English]
Investigating the Role of Soil Physical Properties on Water Infiltration Indices (Case Study: Zanjan Province)
نویسندگان [English]
Mortaza Yavari؛ Alireza Vaezi؛ Mohmmad-Sadegh Askari
Department of Soil Science and Engineering, Faculty of Agriculture, University of Zanjan, Zanjan, Iran
چکیده [English]
Background and Objectives: Infiltration is one of the most important hydraulic properties of soil, representing the entry of water into the soil, which usually occurs in a vertical direction. This soil property plays a crucial role in the natural water cycle and has significant implications for soil management. In semi-arid regions, this hydraulic property is particularly important not only for meeting the water requirements of rangeland and rainfed crops but also for reducing runoff and soil erosion. Several factors influence soil infiltration, and they can be generally categorized into three groups: (1) surface characteristics, (2) soil properties, and (3) climatic and environmental conditions. This study focused on soil physical properties, with the aim of quantifying the influence of a wide range of these properties on water infiltration and identifying the most important factors in selected soils in a semi-arid region.
 

 



Materials and Methods: To investigate the role of soil physical properties on soil water infiltration indices, 68 sites in a semi-arid climate of Zanjan province were selected. To capture sufficient variability for examining the effects of physical factors on soil water infiltration, the sites were chosen based on criteria such as land use type, vegetation cover, and soil texture, ensuring that the experiments were conducted on the predominant soils of the region. At each sampling site, 14 consecutive readings of infiltration depth were recorded at specific time intervals until the infiltration rate reached a steady state flow, for the calculation of various soil water infiltration indices. To evaluate soil water infiltration in detail, six key indices—cumulative infiltration (CI), initial infiltration (II), initial infiltration rate (IIR), final infiltration rate (FIR), mean infiltration rate (MIR), and effective infiltration depth (EID)—were determined. In addition to field infiltration measurements, disturbed and undisturbed soil samples were collected from the 0–60 cm soil depth as the active hydrological layer, and transferred to the laboratory. The following soil physical properties were determined: particle size distribution (PSD), gravel content, bulk density (BD), initial soil moisture, mean weight diameter of dry aggregates (MWDdry), and mean weight diameter and geometric mean diameter of water-stable aggregates (MWDwet and GMDwet).
Results: Pearson correlation analysis revealed that the MWDwet and GMDwet of water-stable aggregates were significantly correlated with all infiltration indices (p< 0.05). Bulk density also exhibited significant correlations with CI, II, FIR, and MIR (p < 0.05). Moreover, multiple regression results indicated that physical properties including BD, initial soil moisture, gravel content, PSD, and GMDwet are the main factors controlling water infiltration in these soils. According to one-way ANOVA, the soils were classified into four groups based on BD, MWDwet, and GMDwet. Significant differences were found among GMDwet groups in CI, II, and FIR (p < 0.05). Differences among the groups of MWDwet in CI and II were significant. Additionally, significant differences were found among the BD groups in CI. This study indicated that, along with soil structure, the particle size distribution of soils can affect soil structure and porosity and, in turn, impact water infiltration in semi-arid soils.

 



Conclusion: The results showed that MWDwet and GMDwet of water-stable aggregates, along with BD, have the highest correlations with soil water infiltration indices. These three soil physical properties can be considered the most important determining factors in explaining soil water infiltration. It was also found that PSD indirectly influences MWDwet, GMDwet, and BD and, consequently, affects soil infiltration behavior. These findings emphasize the importance of PSD and soil structure in the process of soil water infiltration in semi-arid regions.
 

 
کلیدواژه‌ها [English]
Bulk density, Geometric mean diameter, Particle size distribution, Mean weight diameter, Water-stable aggregates
مراجع
  1. Abu‐Hamdeh, N.H., Abo‐Qudais, S.A. and Othman, A.M. 2006. Effect of soil aggregate size on infiltration and erosion characteristics. European Journal of Soil Science, 57(5), 609-616. doi: 1111/j.1365-2389.2005.00743.x
  2. Assouline, S. 2013. Infiltration into soils: Conceptual approaches and solutions. Water Resources Research, 49(4), 1755-1772. https://doi.org/10.1002/wrcr.20155
  3. Assouline, S. 2006. Modeling the relationship between soil bulk density and the hydraulic conductivity function. Vadose Zone Journal, 5(2), 697-705. https://doi.org/10.2136/vzj2005.0084
  4. 2009. Standard test method for infiltration rate of soils in field using double-ring infiltrometer. D3385-09, ASTM International, West Conshohocken, PA.
  5. Basset, C., Abou Najm, M., Ghezzehei, T., Hao, X. and Daccache, A. 2023. How does soil structure affect water infiltration? A meta-data systematic review. Soil and Tillage Research, 226, p.105577. https://doi.org/10.1016/j.still.2022.105577
  6. Beck-Broichsitter, S., Rizvi, Z.H., Horn, R. and Wuttke, F. 2023. Effect of gravel content on soil water retention characteristics and thermal capacity of sandy and silty soils. Journal of Hydrology and Hydromechanics, 71(1), 1-10. https://doi.org/10.2478/johh-2023-0001
  7. Beven, K. and Germann, P. 1982. Macropores and water flow in soils. Water resources research, 18(5). https://doi.org/1311-1325. 0043-1397/82/002 W- 1025 $05.00
  8. Blake, G.R. and Hartge, K.H. 1986. Bulk density. Methods of soil analysis: Part 1 Physical and mineralogical methods, 5, 363-375.
  9. Blanco-Canqui, H. and Ruis, S.J. 2018. No-tillage and soil physical environment. Geoderma, 326, 164-200. https://doi.org/10.1016/j.geoderma.2018.03.011
  10. Bouwer, H. 1986. Intake rate: cylinder infiltrometer. Methods of soil analysis: Part 1 Physical and Mineralogical Methods, 5, 825-844.
  11. Brady, N.C., and Weil, R.R. 2017. The Nature and Properties of Soils, 15th Edn (eBook).
  12. Bronick, C.J., and Lal, R. 2005. Soil structure and management: a review. Geoderma, 124(1-2), 3-22. https://doi.org/10.1016/j.geoderma.2004.03.005
  13. Cerdà, A. 2001. Effects of rock fragment cover on soil infiltration, interrill runoff and erosion. European Journal of Soil Science, 52(1), 59-68. https://doi.org/10.1046/j.1365-2389.2001.00354.xDigital Object Identifier (DOI)
  14. Dane, J.H., and Topp, C.G. (Eds.). 2020. Methods of soil analysis, Part 4: Physical methods. John Wiley and Sons.
  15. Feki, M., Ravazzani, G., Ceppi, A., Milleo, G. and Mancini, M. 2018. Impact of infiltration process modeling on soil water content simulations for irrigation management. Water, 10(7), p.850. DOI:3390/w10070850
  16. Gómez, J.A., Giráldez, J.V., Pastor, M. and Fereres, E. 1999. Effects of tillage method on soil physical properties, infiltration and yield in an olive orchard. Soil and Ttillage Research, 52(3-4), 167-175. https://doi.org/10.1016/S0167-1987(99)00078-1
  17. Hillel, D. 1998. Environmental Soil Physics Academic Press. San Diego, CA.
  18. Hillel, D. 2003. Introduction to environmental soil physics. Elsevier.
  19. Hino, M., Odaka, Y., Nadaoka, K., and Sato, A. 1988. Effect of initial soil moisture content on the vertical infiltration process- A guide to the problem of runoff-ratio and loss. Journal of Hydrology, 102(1-4), 267-284. https://doi.org/10.1016/0022-1694(88)90102-3
  20. Lipiec, J., Medvedev, V.V., Birkas, M., Dumitru, E., Lyndina, T.E., Rousseva, S. and Fulajtar, E. 2003. Effect of soil compaction on root growth and crop yield in Central and Eastern Europe. International agrophysics, 17(2), 61-69.
  21. Horton, R.E. 1940. An approach toward a physical interpretation of infiltration capacity. In Soil science Society of America proceedings Vol. 5, No. 399-417, p. 24. doi:10.2136/sssaj1941.036159950005000C0075X
  22. IUSS Working Group. 2014. World reference base for soil resources 2014. International soil classification system for naming soils and creating legends for soil maps. (No Title).
  23. Jones, J. 2018. Soil analysis handbook of reference methods. CRC press.
  24. Kay, B.P. and Angers, D.A. 1999. Soil structure. In ‘Handbook of soil science’.(Ed. ME Sumner). A-229-A-276.(CRC Press: Boca Raton, USA.).
  25. Lado, M., Paz, A. and Ben-Hur, M. 2004. Organic matter and aggregate size interactions in infiltration, seal formation, and soil loss. Soil Science Society of America Journal, 68(3), 935-942.
  26. Le Bissonnais, Y. 2016. Aggregate stability and assessment of soil crustability and erodibility: I. Theory and methodology. European Journal of Soil Science, 67(1), 11-21. doi:10.1111/ejss.4_12311
  27. Le Bissonnais, Y.L. 1996. Aggregate stability and assessment of soil crustability and erodibility: I. Theory and methodology. European Journal of Soil Science, 47(4), 425-437. doi:10.1111/j.1365-2389.1996.tb01843.x
  28. Li Zhuo, L.Z., Wu Pute, W.P., Feng Hao, F.H., Zhao XiNing, Z.X., Huang Jun, H.J. and Zhuang WenHua, Z.W. 2009. Simulated experiment on effect of soil bulk density on soil infiltration capacity. Transactions of the Chinese Society of Agricultural Engineering, 25(6), 40-45.
  29. Liu, H.L.T.W., Lei, T.W., Zhao, J., Yuan, C.P., Fan, Y.T. and Qu, L.Q. 2011. Effects of rainfall intensity and antecedent soil water content on soil infiltrability under rainfall conditions using the run off-on-out method. Journal of Hydrology, 396(1-2), 24-32.1016/j.jhydrol.2010.10.028
  30. Lv, G. and Wu, X.Y. 2008. Review on influential factors of soil infiltration characteristics. Chinese Agricultural Science Bulletin, 24, 494-499. doi:10.11924/j.issn.1000-6850.20080196
  31. Morbidelli, R., Corradini, C., Saltalippi, C., Flammini, A., Dari, J., and Govindaraju, R.S. 2018. Rainfall infiltration modeling: A review. Water, 10(12), 1873. doi:10.3390/w10121873.
  32. Sedayeeazar, Z., Mohammadi, M. H., Asadi, H. 2025. The effect of gravel on the cumulative infiltration in two different soil textures. Iranian Journal of Soil and Water Research, 55(12), 2483-2498. doi: 10.22059/ijswr.2024.379854.669763. (in Persian)
  33. Talat, A.E., Feng, R., Liu, G., Xie, J., Cai, Z. and Wang, J. 2025. Simulated experimental effect of bulk density on infiltration rate of China’s loess plateau. Egyptian Journal of Soil Science, 65(1). doi:10.21608/ejss.2024.328370.1886.
  34. Turner, E. 2006. Comparison of infiltration equations and their field validation by rainfall simulation. University of Maryland, College Park.
  35. Vaezi, A.R., Behtari, M., and Foroumadi, M. 2019. Time variations of rainfall infiltration into the soil under the influence of soil initial moisture. Iranian Journal of Irrigation and Drainage, 13(3 ), 575-587. (in Persian)
  36. Vaezi, A.R. 2018. Water Erosion: Processes and Models. 4th University of Zanjan Press, Zanjan, Iran, 513. (in Persian)
  37. Xu, C., Liu, W., Li, J., Wu, J., Zhou, Y. and Kader, R. 2024. Dynamic change of soil aggregate stability and infiltration properties during crop growth under four tillage measures in Mollisols region of northeast China. Frontiers in Earth Science, 12, p.1357467. doi:10.3389/feart.2024.1357467
  38. Yang, T., Zhang, Z., Yu, P., Yin, Z., Li, A., Zhou, X., Qi, Z. and Wang, B. 2024. Soil aggregates and water infiltration performance of different water and soil conservation measures on phaeozems sloping farmland in northeast China. Agronomy, 14(10), p.2410. doi:10.3390/agronomy14102410.
  39. Yavari, M., Mohammadi, M. H., Shahbazi, K. 2021. Comparison of some methods for measuring primary soil particle size distribution and introducing appropriate times for the four-reading method for determining soil texture. Iranian Journal of Soil and Water Research, 51(12), 2999-3015. doi: 10.22059/ijswr.2020.310061.668738. (in Persian)
  40. Yavari, M., Mohammadi, M., Shahbazi, K. 2020. The effect of cement removal in measuring the texture of Iran soils. Iranian Journal of Soil and Water Research, 51(8), 1947-1958. doi: 10.22059/ijswr.2020.280297.668188. (in Persian)
  41. Yılmaz, E., Çanakcı, M., Topakcı, M., Sönmez, S., Ağsaran, B., Alagöz, Z., Çıtak, S. and Uras, D.S. 2019. Effect of vineyard pruning residue application on soil aggregate formation, aggregate stability and carbon content in different aggregate sizes. Catena, 183, p.104219. doi:10.1016/j.catena.2019.104219
  42. Zeng, J., Fei, L.J. and Pei, Q.B. 2017. Influence of soil bulk density on soil water infiltration characteristics in water vertical movement. Journal of Drainage and Irrigation Machinery Engineering, 12(35), 1081-1087. doi:10.3969/j.issn.1674‑8530.16.0294
  43. Zewide, I. 2021. Review paper on effect of natural condition on soil infiltration. Chemistry, 7(1), 34-41p. doi: 10.37628/IJGC
  44. Zhang, H., Niu, L.A., Hu, K., Hao, J., Li, F., Gao, Z. and Wang, X. 2020. Influence of tillage, straw-returning and mineral fertilization on the stability and associated organic content of soil aggregates in the North China Plain. Agronomy, 10(7), p.951. doi: 3390/agronomy10070951
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