ارزیابی وتعیین مؤثرین شاخص برحساسیت خاک به تشکیل اندوده سطحی با بهره‌گیری از رگرسیون ریج

نویسندگان

1 دانشگاه تبریز

2 دانشیار دانشگاه تبریز

3 عضو هیئت علمی دانشگاه تبریز

4 استادیار مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی فارس

5 دانشیار گروه اصلاح و نباتات دانشگاه سراسری تبریز

چکیده

تحقیق حاضر برای شناسایی شاخصی کارآمد برای تعیین حساسیت خاک به تشکیل اندوده در منطقه دشت کوار استان فارس انجام شد. برای انجام این تحقیق80 نمونه مرکب خاک (20-0 سانتی‌متری) از دشت کوار استان فارس تهیه گردید. سپس پارامترهای توزیع اندازه ذرات خاک، رطوبت جرمی، ماده آلی، هدایت الکتریکی و pH عصاره گل اشباع اندازه‌گیری شدند. همچنین میانگین وزنی قطر خاکدانه‌ها، میانگین هندسی قطر خاکدانه‌ها، کربنات کلسیم معادل، بعد فرکتالی، درصد اشباع ، سدیم، کلسیم، منیزیم، نسبت جذب سطحی سدیم، هدایت هیدرولیکی اشباع و جرم مخصوص ظاهری خاک تعیین ‌شد. ارزیابی حساسیت خاک به تشکیل اندوده با مقایسه معادله های رگرسیونی هفت شاخص مختلف از جمله شاخص پایداری ساختمان خاک (SSI)، شاخص سله‌بندی (CI)، شاخص پایداری خاکدانه مرطوب (WAS)، شاخص حساسیت به سله بستن (CSI)، شاخص پایایی (C5- C10)، مقاومت در برابر نفوذ (PR) و شاخص نسبی اندوده بستن (RSI) انجام و برای تحلیل داده‌ها از روش همبستگی پیرسون و رگرسیون خطی چندگانه ریج به روش گام به گام پس رونده و با استفاده از نرم‌افزارهای Statistica، SPSS-26 و Minitab استفاده گردید. در مطالعه حاضر بهترین مدل‌‌های رگرسیونی برازش داده شده جهت توصیف حساسیت پذیری خاک به تشکیل اندوده سطحی متعلق به شاخص های پایداری خاکدانه و سله‌بندی فائو بودند. بر اساس نتایج حاصله شاخص پایداری خاکدانه با ضریب تبیین اصلاح شده 92/0 R2 adj=در پیش بینی حساسیت خاک به تشکیل اندوده قابلیت بالایی داشت و مؤثرترین شاخص در بیان تغییرات پایداری خاکدانه و تشکیل اندوده سطحی بود.

کلیدواژه‌ها


عنوان مقاله [English]

Evaluation and Determination of the Most Effective Index on Soil Sensitivity to the Surface Sealing Using Ridge Regression

نویسندگان [English]

  • Zhila Asadi Fard 1
  • Abbas Ahmadi 2
  • Ali Asghar Jafarzadeh 3
  • alidad karami 4
  • Siamak AlaviKia 5
1 دانشجو
2 Associated Professor
3 University of Tabriz Academic Member
4 Assistant professor of Fars Center for Research and Education of Agricultural Science and Natural Resources
5 Associate Professor, Department of Plant Breeding, University of Tabriz
چکیده [English]

Abstract:
Background and Objectives:

The surface seal formation can have destructive agricultural, hydrological and environmental effects. Seal formation is a complex mechanism that controlled by a wide range of factors such as soil properties, rainfall characteristics, and flow conditions. The present research was conduct in order to identify an efficient index to determine the sensitivity of soil to the seal formation in the soil of Kowar plain region of Fars province.
Methodology
In the present study, according to the area of the region, 160 sampling points selected, then according to the characteristics of the studied area and type of land use, to achieve the goals of the research, first, the land use, geology and topography maps of the area is prepared and by doing several times of field work in different seasons of the year, the topographies and shapes in the maps and pictures were adapted to the environmental conditions. To carry out this research, 80 composite soil samples (0-20 cm) were prepared from the Kovar plain of Fars province. Then the parameters of soil particle size distribution, mass moisture, organic matter, electrical conductivity and pH of saturated mud extract measured. Then the parameters of soil particles size distribution, volume wetness, organic matter, electrical conductivity and pH of saturated mud extract, measured. Also, mean weight diameter(MWD), geometric mean diameter(GMD), calcium carbonate equivalent, fractal dimensions, saturation percentage, sodium, calcium, magnesium, sodium absorption ratio (SAR), saturated hydraulic conductivity (Ks) and bulk density were determined. Assessing the sensitivity of the soil to the surface seal formation by comparing the regression equations of seven different indices, including the soil structural stability index (SSI), crusting index (CI), water aggregate stability (WAS), crusting susceptibility index (CSI), consistency index (C5 - C10), penetration resistance (PR) and relative sealing index (RSI) carried out in data preprocessing, Descriptive statistics of variables such as mean, maximum, minimum and variance, data distribution diagram and data distribution obtained using Minitab- 19 software. In addition, in case of remote data or mistakes in entering the data, appropriate measures taken and a table of descriptive information was prepared. The normality of the frequency distribution of these features evaluated using the significance test of skewness. To explain the ability of indicators and statistics in seal formation, First, linear correlation between variables determined by SPSS-22 software and by using Pearson's correlation coefficient (r), the correlation relationship between the indices and early characteristics of the soil was obtained and for data analysis, Pearson's correlation method and ridge multiple linear regression were used by stepwise backward method and using Statistica, SPSS-26 and Minitab-19 software.



Findings:
In terms of the soil structural stability index, the studied area was in the danger range of aggregate destruction, which can considered relevant to the high percentage of silt in the region. The sodium surface absorption ratio of the majority of soil samples in the study area, had a non-sodium rating. 95% of the samples with agricultural land use in terms of organic matter were located in the weak to medium with structure and structure stability group. The majority of samples had more than 20% clay. Most of the measured variables had a low coefficient of variation and in terms of data distribution and dispersion, had a relatively favorable situation. Clay was the common variable in five regression equations of the indices, which refers to the importance and dual role of clay in the aggregates stability and reducing the sensitivity to compaction. The relatively low value of the standard deviation in the soil structural stability index indicated the greater accuracy of this model in estimating the coefficients. In the present study, the best-fitted regression model, to describe the sensitivity of the soil to the surface seal formation, compared to other models, belong to the soil structural stability and crusting indices.

Conclusion:
Based on the results obtained, the soil aggregate stability index with the modified coefficient of explanation R2=0.92 had a high capability in predicting the sensitivity of the soil to the seal formation and is the most effective index in expressing the changes in soil aggregate stability and the surface sealing. The results of the data analysis expressing the extreme limitation class of the mean weight diameter was in the soil of the region.

کلیدواژه‌ها [English]

  • Aggregate stability
  • Regression model
  • Ridge multivariate regression
  • Sealing surface
  • Soil quality
Abulhasan Beigi A, 2004. Agricultural climate of Kovar plain in Fars province with emphasis on wheat cultivation, Iran. MSc Thesis in natural geography, Isfahan University. (In Persian with English abstract)
Arjmand Sajjadi S and Mahmoodabadi M, 2015. Aggregate breakdown and surface seal development influenced by rain intensity, slope gradient and soil particle size. Published by Copernicus Publications on behalf of the European Geosciences Union 6: 311–321.
Assouline S, 2004. Rainfall-induced soil surface sealing: A critical review of observations, Conceptual models and solutions. Soil Science Society of America. Vadose Zone Journal 3: 570–591.
Assouline S and Mualem Y, 2006. Runoff from heterogeneous small bare catchments during soil surface sealing, Water Resources Research 42: 1-11.
Assouline S, Selker JS and Parlange JY, 2007. A simple accurate method to predict time of ponding under variable intensity rainfall. Water Resources Research 43:1-10.
Ben-Hur M and Letey J, 1989. Effect of polysaccharides, clay dispersion and impact energy on water infiltration. Soil Science Society of America Journal 53: 233–238.
Bohn HL, McNeal BL and O`Coner GA, 1996. Soil nutrients and salinity after long-term grazing exclusion in a flooding pampa grassland. Journal of Rang Management 49: 182-187.
Canasveras JC, Barron V, Del Campillo MC, Torrent J and Gomez JA, 2010. Estimation of aggregate stability indices in Mediterranean soils by diffuse reflectance spectroscopy. Geoderma 158: 78-84.
Emerson WW, 1977. Physical properties and structure. Soil factors in crop production in a semi-arid environment. Pp. 78–104. In: Russell JS and Greacen EL (eds). University of Queensland Press, St. Lucia, QLD, Australia.
FAO/UNESC0, 1974. Soi1 Map of the World, 1:5 000 000. Legend. Vol, 1. Paris. UNESCO.
Gee GW and Or D, 2002. Particle-size analysis. Pp. 255-295. In: Warren AD (ed.) Methods of Soil Analysis. Part 4. Physical Methods, Soil Science Society of American Journal. Inc.
Hajabbasi MA, 1999. Methods and Guidelines for Assessing Sustainable Use of Soil Water Resources in the Tropics. Ferdowsi University of Mashhad Publication.
Hoerl AE and Kennard RW, 1970a. Ridge regression, biased estimation for non-orthogonal problem. Technometrics Journal 12: 55-67.
Hoerl AE and Kennard RW, 1970b. Ridge regression: applications to non-orthogonal problems. Technometrics Journal 12: 69-82.
Jenerette GD, Barron-Gafford GA, Guswa AJ, McDonnell JJ and Camilo Villegas J, 2012. Organization of complexity in water limited ecohydrology Ecohydrology Journal 5: 184–199.
Kemper WD and Rosenau RS, 1986. Aggregate stability and size distribution. Pp. 425-442. In: Klute A (eds). Methods of Soil Analysis, Part I: Physical Analysis. Soil Science Society of American Journal. Madison Wisconsin.
Manyevere A, Bangira C, Gotosa J, Munjonji L and Chikwari E, 2015. Characteristics and management options of crusting soils in a smallholder farming area of the Zambezi metamorphic belt in northern Zimbabwe. South African Journal of Plant and Soil 32: 157–164.
Moncada MP, Gabriels D, Lobo D, Beuf K, Figueroa R and Cornelis WM, 2014. A comparison of methods to assess susceptibility to soil sealing. Geoderma 226-227: 397-404.
Nelson RE, 1982. Carbonate and gypsum. Pp. 181-199. In: Page L.A (ed.). Methods of Soil Analysis, part 2. American Society of Agronomy Journal, Madison.
Nelson DW and Sommer LE, 1982. Total carbon, organic carbon and organic matter. Pp. 961-1069. In: Sparks DL, Helmke PA, Loeppert RH, Soltanpour PN, Tabatabai MA and Johnston, CT (eds). Methods of Soil Analysis: part3, Chemical Methods. American Society of Agronomy Journal, Madison.
Nimmo JR and Perkins KS, 2002. Aggregate stability and Size distribution. Pp. 317-328. In: Warren AD (ed.). Methods of Soil Analysis. Part 4. Physical Methods. American Society of Agronomy Journal, Madison.
Peyvasteh F, Asadi H and Akef M, 2010. The relationship between soil grain stability and surface layer formation and its effect on soil erosion in laboratory conditions: Journal of Watershed Sciences and Engineering 10: 1 - 8. (In Persian with English abstract)
Pieri C, 1989. Fertilite des Terres de Savane. Bilan de Trente Ans de Recherché et de Development Agricoles au Sud du Sahara. Ministère de la Cooperation/Cirad, Paris.
Pla I, 1986. A routine laboratory index to predict the effect of soil sealing on soil and water conservation. Pp. 154-162. In: Callebaut F, Gabriels D and De Booodt M (eds.). Assessment of Soil Sealing and Crusting. Proceedings of the Symposium Held in Ghent, Belgium.
Rieu M and and Sposito G, 1991. Fractal fragmentation, soil porosity and soil water properties. Π. Aplications. Soil Science Society of America Journal 5: 1239-1244.
Schwartz RC, Baumhardt RL and Evett SR, 2010. Tillage effects on soil water redistribution and bare soil evaporation throughout a season. Soil Tillage Research Journal 110: 221–229.
Sela Sh, Svorary T and Assouline Sh, 2012. Soil water content variability at the hillslope scale, Impact of surface sealing. Water Resources Research Journal 48:1-14.
Sela Sh, Svorary T and Assouline Sh, 2015. The effect of soil surface sealing on vegetation water uptake along a dry climatic gradient. Water Resources Research Journal 51: 7452-7466.
Shahab H, Emami H, Haghnia GH and Karimi A, 2011. Determining most important properties for soil quality indices of agriculture and range lands in some parts of Southern Mashhad. Journal of Water and Soil 25:1197-1205. (In Persian with English abstract)
Topp GC, Reynolds WD, Cook FJ, Kirby JM and Carter MR, 1997. Physical attributes of soil quality. Pp. 21-58. In: Gregorich EG and Carter MR (eds.) Soil Quality for Crop Production and Ecosystem Health. Elsevier Science Journal, Amsterdam.
Wang D, Fu B, Zhao W, Hu H and Wang Y, 2008. Multifractal characteristics of soil particle size distribution under different land-use types on the Loess Plateau. Science Direct Journal 72:29-36.
Wang Q, Zhang T, Cui J, Wang X, Zhou H, Han J and Gislum R, 2011. Path and ridge regression analysis of seed yield and seed yield components of Russian wildrye (Psathyrostachys juncea Nevski) under field conditions. Plos One 6: 1-10.