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بررسی رابطه بین آبگریزی طبیعی و ویژگی‌های فیزیکو شیمیایی خاک در کاربری‌های مختلف در مناطق ساحلی غرب گیلان | ||
| تحقیقات آب و خاک ایران | ||
| دوره 52، شماره 7، مهر 1400، صفحه 1807-1823 اصل مقاله (1.12 M) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/ijswr.2021.323653.668972 | ||
| نویسندگان | ||
| سیده مهرنوش میربابایی1؛ محمود شعبانپور شهرستانی* 2؛ محمد رضا خالدیان3؛ علی اصغر ذوالفقاری4 | ||
| 1دانشجوی دکتری، گروه خاکشناسی، دانشکده علوم کشاورزی، دانشگاه گیلان، رشت، ایران | ||
| 2دانشیار گروه خاکشناسى، دانشکده کشاورزى، دانشگاه گیلان، رشت | ||
| 3دانشیار گروه مهندسی آب، دانشکده علوم کشاورزی، دانشگاه گیلان، رشت، ایران | ||
| 4دانشیار گروه بیابان زدایی، دانشکده کویرشناسی، دانشگاه سمنان، سمنان، ایران | ||
| چکیده | ||
| آبگریزی خاک یک خصوصیت دینامیک است که نفوذ آب به خاک را به تاخیر انداخته و پتانسیل ایجاد رواناب و فرسایش را افزایش می‌دهد. دانش دقیق در مورد وجود و شدت آبگریزی مناطق ساحلی گیلان، که تحت کاربری‌های مختلف اراضی هستند، از اهمیت خاصی برخوردار است. مطالعه حاضر اثر کاربری اراضی را بر آبگریزی خاک در سه منطقه 1) منطقه جنگلکاری شده با پوشش کاج تدا 2) منطقه‌ی جنگلکاری شده با کاج تدا و در برخی قسمت‌ها تحت پوشش طبیعی انار وحشی 3) زمین کشاورزی تحت پوشش خرمالو ارزیابی می‌کند. آبگریزی خاک با سه آزمون زمان نفوذ قطره آب، مولاریته قطره اتانول و منطقه خیس شده خاک اندازه‌گیری شد. همچنین رابطه بین آبگریزی و برخی از خصوصیات (ماده آلی خاک، اسیدیته، نیتروژن کل، فسفر قابل استفاده، ظرفیت تبادل کاتیونی، قابلیت هدایت الکتریکی، سدیم، پتاسیم، کلسیم، منیزیم، بافت خاک، جرم مخصوص ظاهری و حقیقی) در 200 نمونه بررسی شد. شدت آبگریزی در 6 سایز اندازه ذرات (2-1، 5/0-1، 25/0-5/0، 125/0-25/0، 125/0-05/0 و 05/0> میلی‌متر) ارزیابی شد. بر اساس نتایج، خاک‌های تحت پوشش کاج تدا بیشترین آبگریزی و خاک‌های تحت پوشش انار وحشی و کشت شده با خرمالو کمترین آبگریزی را نشان دادند. همچنین ماده آلی و نیتروژن کل با اثر مثبت و اسیدیته خاک با اثر منفی مهم‌ترین پارامترهای کنترل کننده آبگریزی در این خاکها بودند. نتایج نشان دادند اگرچه خاک‌های درشت بافت برای ایجاد آبگریزی مستعدتر هستند اما کوچک‌ترین اندازه ذرات در این خاکها نقش بسیار مهمی در شدت آبگریزی خاک دارد. | ||
| کلیدواژه‌ها | ||
| آبگریزی خاک؛ زمان نفوذ قطره آب؛ مولاریته قطره اتانول؛ منطقه خیس شده خاک | ||
| عنوان مقاله [English] | ||
| Investigation of the Relationship between Natural Hydrophobicity and Physicochemical Properties of Soil in Different Land Uses in the Coastal Areas of West Guilan | ||
| نویسندگان [English] | ||
| Seyedeh Mehrnoosh Mirbabaei1؛ Mahmoud Shabanpour2؛ Mohammadreza Khaledian3؛ Aliasghar Zolfaghari4 | ||
| 1pH.D. Student, Department of Soil Science, University of Guilan, 41635-1314, Rasht, Iran | ||
| 2Department of Soil Science, University of Guilan, 41635-1314, Rasht, Iran | ||
| 3Department of Water Engineering, University of Guilan, 41635-1314, Rasht, Iran | ||
| 4Department of Desert Science, University of Semnan, Semnan, Iran | ||
| چکیده [English] | ||
| Soil water repellency is a dynamic property that delays the infiltration of water into the soil and increases the potential for runoff and erosion. Accurate knowledge about the existence and severity of soil water repellency (SWR) in the coastal areas of Guilan, which are under different land uses, is very important. The present study evaluates the effects of land uses on soil water repellency in three areas: 1) Forested area with Pinus Teda, 2) forested area planted with Pinus Teda in some parts and covered with natural wild pomegranate in other parts 3) Agricultural land covered with Diaspyros Kaki. Soil water repellency was measured using three tests of the water drop penetration time (WDPT), the molarity of ethanol droplet (MED) and the soil wetted area (SWA). Significant differences in soil water repellency were found among the different land uses. Forest soils under pinus Teada showed the highest SWR and the soils under wild pomegranate and persimmon cultivated area showed the lowest SWR. Also, the relationship between SWR and soil properties (soil organic matter, pH, total nitrogen, phosphorus, Cation Exchangable Capacity, Electrical Conductivity, sodium, potassium, calcium, magnesium, soil texture, bulk and particle density) was investigated in 200 samples. Principal component analysis (PCA) showed that organic matter, total nitrogen with a positive effect and soil acidity with a negative effect are the most important parameters controlling repellency in these soils. To investigate which component of the soil particles have a more important role in creating water repellency, the intensity of water repellency was examined in six particle sizes of the soil (1-2, 0.5-1, 0.25-0.5, 0.125-0.25, 0.05-0.125 and less than 0.05 mm). The results showed that although coarse-textured soils are more prone to repellency, the smallest particle size in these soils plays a very important role in the intensity of soil water repellency. | ||
| کلیدواژه‌ها [English] | ||
| Soil Water Repellency, Water Drop Penetration Time, Molarity of Ethanol, soil wetted area | ||
| مراجع | ||
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Alanis, N., Hernandez-Madrigal, V. M., Cerda, A., Munoz-Rojas, M., Zavala, L. M. and Jordan, A. (2017). Spatial gradients of intisity and persistence of soil water repellency under different forest types central Mexico. Land Degrad. Develop, 28, 317–327. Atanassova, I. and Doerr, S. H. (2011). Changes in soil organic compound composition associated with heat-induced increases in soil water repellency. Eur. J. Soil Sci. 62 (4), 516–532. Atanassova, I., Banov, M., Shishkov, T., Petkova, Z., Hristov, B., Ivanov, P., Markov, E., Kirilov, I. and Harizanova, M. (2018). Relationships between soil water repellency, physical and chemical properties in hydrophobic technogenic soils from the region of maritsa-iztok coal mine in Bulgaria. Bulgarian Journal of Agricultural Science, 24 (2), 10-17. Bisdom, E. B. A., Dekker, L. W. and Schoute, J. F. Th. (1993). Water repellency of sieve fractions from sandy soils and reletionships with organic material and soil structure. Geoderma 56, 105-118. Bonanomi, G., Gaglione, S. A., Antignani, V. and Cesarano, G. (2016). Unimodal pattern of soil hydrophobicity along an altitudinal gradient encompassing Mediterranean, temperate, and alpine ecosystems. Plant Soil, 409 37–47. Bremner, J. M., and Mulvaney, C. S. (1982). Totalnitrogen. In: A. L. Page (Ed.) Methods of SoilAnalysis. P Part 2: Chemical and microbiologicalproperties (2th Ed.). Agron. (No.2). pp.95-624. Madison, Wisconsin, USA: Soil Science Society of America. Brevik, E. C., Cerda, A., Mataix-Solera, J., Pereg, L., Quinton, J. N., Six, J. and Van Oost, K. (2015). The interdisciplinary nature of SOIL. Soil, 1, 117-129. Buczko, U., Bens, O., Fischer, H. and Huttl, R. F. (2002). Water repellency in sandy luvisols under different forest transformation stages in northeast Germany. Geoderma, 109, 1-18. Carrick, S., Buchan, G., Almond, P. and Smith, N. (2011). Atypical early-time infiltration into a structured soil near field capacity: the dynamic interplay between sorptivity, hydrophobicity, and air encapsulation. Geoderma 160 (3–4), 579–589. Chau, H. W., Biswas, A., Vujanovic, V. and Cheng Si, B. (2014). Relationship between the severity, persistence of soil water repellency and the critical soil water content in water repellent soils. Geoderma 221–222, 113–120. Clark, E. V. and Zipper, C. E. (2016). Vegetation influences near-surface hydrological characteristics on a surface coal mine in eastern USA. Catena, 139, 241–249. Daniel, N. R. R., Uddin, S. M. M., Harper, R. J. and Henry, D. J. (2019). Soil water repellency: A molecular-level perspective of a global environmental phenomenon. Geoderma 338, 56–66. Davies, B. E. (1974). Loss-on- Ignition as an estimate of soil organic matter, Soil Sci. Am. Proc. 38, 150-151. DeBano, L. F. (1981). Water Repellent Soils: A State-of-the-Art. Dekker, L. W and Ritsema, C. J. (2000). Wetting patterns and moisture variability in water repellent Dutch soils. J Hydrol, 231-232:148–164. Dekker, L. W. and Ritsema, C. J. (1994). How water moves in a water-repellent sandy soil. I. Potential and actual water repellency. Water Resour. Res, 30, 2507–2517. Dekker, L. W.; Oostindie, K and Ritsema, C. J. (2005). Exponential increase of publications related to soil water repellency. Aust. J. Soil Res, 43, 403–441. Diehl, D. (2013). Soil water repellency: dynamics of heterogeneous surfaces. Colloids Surf. A Physicochem. Eng. Asp. 432, 8–18. Doerr, S. H. and Moody, J. A. (2004). Hydrological effects of soil water repellency: on spatial and temporal uncertainties. Hydrol. Process, 18, 829–832. Doerr, S. H., Dekker, L. W., Ritsema, C. J., Shakesby, R. A. and Bryant, R. (2002). Water repellency of soils: the influence of ambient relative humidity. Soil Sci. Soc. Am. J. 66 (2), 401–405. Doerr, S. H., Shakesby, R. A. and Walsh, R. P. D. (1998). Spatial variability of soil hydrophobicity in fire-prone eucalyptus and pine forests, Portugal. Soil Sci. 163, 313–324. Doerr, S. H., Shakesby, R. A. and Walsh, R. P. D. (2000). Soil water repellency: its causes, characteristics and hydro-geomorphological significance. Earth Sci. Rev. 51, 33–65. Fer, M., Leue, M., Kodesova, R., Gerke, H. H and Ellerbrock, R. H. (2016). Droplet infiltration dynamics and soil wettability related to soil organic matter of soil aggregate coatings. J. Hydrol. Hydromech, 64: 111–120. Flint, A. and Flint, L. (2002). Particle density. In: Dane, J.H. and Topp, G. C. (Eds.), Methods of soil analysis, Part 4- Physical methods. Agronomy Monograph, vol. 9. ASA and SSSA, Madison, WI, PP 229-240. Flores-Mangual, M. L., Bockheim, B. L. J. G., Pagliari. P. H. and Scharenbroch, B. (2013). Hydrophobicity of Sparta Sand under Different Vegetation Types in the Lower Wisconsin River Valley. Soil Sci. Soc. Am. J. 77, 1506–1516. Flores-Mangual, M. L., Lowery, B., Bockheim, J. G. Bockheim and Pagliari, P. H. (2011). A revised water drop method for assessing soil water repellency. Soil Sci. 176(3), 124–128. Franco, C. M. M., Tate, M. E. and Oades, J. M. (1995). Studies on non-wetting sands. I. the role of intrinsic particulate organic-matter in the development of water-repellency in non-wetting sands. Aust J Soil Res, 33:253–263. Gao, Y., Lin, Q., Liu, H., Wu, H., Alamus. (2018). Water repellency as conditioned by physical and chemical parameters in grassland soil. Catena, 160, 310–320. Garcia-Moreno, J., Gordillo-Rivero, A. J., Zavala, L. M., Jordan, A. and Pereira, P. (2013). Mulch application in fruit orchards increases the persistence of soil water repellency during a 15-years period. Soil Tillage Res, 130, 62–68. Gee, G. W. and Or, D. (2002). Particle-size analysis. In: Dane, J.H., Topp, G.C. (Eds.), Methods of soil analysis, part 4 — physical methods. : Agronomy Monograph, vol. 9. ASA and SSA, Madison, WI pp, 255–293. Goebel, M. O., Bachmann, J., Reichstein, M., Janssens, I. A. and Guggenberger, G. (2011). Soilnwater repellency and its implications for organic matter decomposition – is there a link to extreme climatic events? Glob. Chang. Biol, 17 (8), 2640-2656. Hallett, P. D. (2008). A brief overview of the causes, impacts and amelioration of soil water repellency–a review. Soil Water Res, 3, 21–29. Jimenez-Morillo, N. T., Gonzalez-Perez. J. A., Jordan, A., Zavala, L. M., Maria de la Rose, J., Jimenez-Gonzalez, M. A. and Gonzalez-Vila, F. J. (2014). Organic material fractions controlling soil water repellency in sandy soils from the Donana national park (southwestern Spain). Land Degrad. Develop. 27, 1413–1423 Jordan, A., Zavala, L. M., Mataix-Solera, J. and Doerr, S. H. (2013). S Soil water repellency: origin, assessment and geomorphological consequences. Catena, 108, 1–8. Kaiser, H. (1974). An index of factorial simplicity. Psychometrika, 39, 31–36. Kaiser, M., Kleber, M. and Berhe, A. (2015). How air-drying and rewetting modify soil organic matter characteristics: an assessment to improve data interpretation and inference. Soil Biol Biochem, 80, 324–340 Klute, A. (1986). Method of Soil Analysis. Part. 1. Physical and Mineralogical Methods. Soil. Sci. of America. Madison, Wisconsin. USA. Leelamanie, D. A. L. (2016). Occurrence and distribution of water repellency in size fractionated coastal dune sand in Sri Lanka under Casuarina shelterbelt. Catena, 142, 206-212. Letey, J. and Pelishek, R. E. (1962). Measurement of liquid-solid contact angles in soil and sand. Soil Sci. 93(3):149-153. Lichner, L., Hallett, P. D., Feeney, D. S., Dugov, A. O., Sir, M. and Tesar, M. (2007). Field measurement of soil water repellency and its impact on water flow under different vegetation. Biologia, 62, 537–541. Lucas-Borja, M. E., Zema, D. A., Plaza-Alvarez, P. A., Zupanc, V., Baartman, J., Sagra, J., Gonzalez-Romero, J. Moya , D. and de las Heras , J. (2019). Effects of Different Land Uses (Abandoned Farmland, Intensive Agriculture and Forest) on Soil Hydrological Properties in Southern Spain. Water 11, 503-518. Mao, J. (2016). Water repellent soils: from molecule to ecosystem. PhD dissertation Utrecht University, Utrecht, the Netherlands, 186 pp Mao, J., Nierop, K. G. J., Dekker, S. C., Dekker, L. W. and Chen, B. (2019). Understanding themechanisms of soil water repellency from nanoscale to ecosystem scale: a review. J. Soils Sediments 19, 171–185. Mao, J., Nierop, K. G. J., Rietkerk, M. and Dekker, S. C. (2015). Predicting soil water repellency using hydrophobic organic compounds and their vegetation origin. Soil 1, 411–425. Mao, J., Nierop, K. G. J., Sinninghe Damste, J. S and Dekker, S.C. (2014). Roots induce stronger soil water repellency than leaf waxes. Geoderma, 232-234:328–340 Mataix-Solera, J., Arcenegui, V., Zavala, L. M., Perez-Bejarano, A., Jordan, A., Morugan-Coronado, A., Barcenas-Moreno, G., Jimenez-Pinilla, P., Lozano, E., Granged, A. J. P., Gil-Torres, J. (2014). Small variations in soil properties control fire-induced water repellency. Spanish Journal of Soil Science 4, 51–60. Moreno-de las Heras, M., Merino-Martin, L. and Nicolau, J. M. (2009). Effect of vegetation cover on the hydrology of reclaimed mining soils under Mediterranean-Continental climate. Catena, 77, 39–47. Morley, C. P., Mainwaring, K. A. Doerr, S. H., Douglas, P., Llewllyn, C. T. and Dekker, L. W. (2005). Organic compounds at different depths in a sandy soil and their role in water repellency. Aust. J. Soil Res, 43,239-249. Olsen, S. R. and Sommers, L. E. (1982). Phosphorus, In: Page, A.L., Miller, R.H., Keeny, D.R. (Eds.), Methods of soil analysis. Part 2. Chemical andmicrobiological properties, 2nd edition. Agronomy Monograph, 9. American Society of Agronomy, Soil Science Society of America, Madison, WI, pp. 403–430. Pallant, J. (2005). SPSS survival manual: a step by step guide to data analysis using spss. Buckingham: allen & unwin. Rhoades, J. D. (1996). Salinity: Electrical conductivity and total dissolved solids. In: Sparks, D.L.,(Eds.), Methods of soil analysis, Part 3- Chemical Methods. Agronomy Monograph, vol. 9. ASA and SSSA, Madison, WI, pp 417-435. Ritsema, C. J., Van Dam, J. C., Dekker, L. W. and Oostindie, K. (2005). A new modelling approach to simulate preferential flow and transport in water repellent porous media: Model structure and validation. Australian Journal of Soil Research, 43, 36-369. Schnabel, S., Pulido-Fernandez, M. and Lavado-Contador, J. F. (2013). Soil water repellency in rangelands of Extremadura (Spain) and its relationship with land management. Catena, 103, 53–61. Scott, D. F. (2000). Soil wettability in forested catchments in South Africa; as measured by different methods and as affected by vegetation cover and soil characteristics. J. Hydrol, 231–232, 87–104. Sumner, M. E. and Miller, W. P. (1996). Cation exchange capacity and exchange coefficients. Methods of Soil Analysis Part 3-Chemical Methods, (methodsofsoilan3). (Pp.1201-1229). Thomas, G.W. (1996). Soil pH and soil activity. In. Sparks, D.L.,(Eds), Methods of soil analysis, Part 3- Chemical Methods.Agronomy Monograph, vol. 9. ASA and SSSA, Madison, WI, pp 475-490. Wallis, M. G. and Horne, D. J. (1992). Soil water repellency. In Advances in Soil Science; Stewart, B.A., Ed.; Springer: New York, NY, USA, Volume 20, pp. 91–146. Wessolek, G., Stoffregen, H. and Taumer, K. (2009). Persistency of flow patterns in a water repellent sandy soil: conclusions of TDR readings and a time delayed double tracer experiment. Journal of Hydrology 375, 524–535. Zavala, L. M. and Jordan-Lopez, A. (2009). Influence of different plant species on water repellency in Mediterranean heathland soils. Catena, 76, 215–223. Zavala, L. M., Garcia-Moreno, J., Gordillo-Rivero, A., Jordan, A., Mataix-Solera, J. (2014). Natural soil water repellency in different types of Mediterranean woodlands. Geoderma, 226–227, 170–178. Zema, D. A., Plaza-Alvarez, P. A., Xu, X., Gianmarco Carra, B. and Lucas-Borja, M. E. (2021). Influence of forest stand age on soil water repellency and hydraulic conductivity in the Mediterranean environment. Science of the Total Environment, 753. 142006 Zheng, W., Morris, E.K., Lehmann, A. and Rillig, M.C. (2016). Interplay of soil water repellency, soil aggregation and organic carbon. A meta-analysis. Geoderma, 283, 39–47.
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