| تعداد نشریات | 24 |
| تعداد شمارهها | 874 |
| تعداد مقالات | 7,803 |
| تعداد مشاهده مقاله | 14,218,001 |
| تعداد دریافت فایل اصل مقاله | 12,164,653 |
The study of particle size distribution of calcium carbonate and its effects on some soil properties in khuzestan province | ||
| Iran Agricultural Research | ||
| مقاله 10، دوره 36، شماره 2، اسفند 2017، صفحه 71-80 اصل مقاله (500.82 K) | ||
| نوع مقاله: Full Article | ||
| شناسه دیجیتال (DOI): 10.22099/iar.2017.4147 | ||
| نویسندگان | ||
| N. Asgari Hafshejani* ؛ S. Jafari | ||
| Department of Soil Science, Ramin University of Agriculture and Natural Resources, Ahvaz University,Ahvaz, I.R. Iran | ||
| چکیده | ||
| ABSTRACT-This experiment was carried out to study particle size distribution (PSD) of carbonates in soils and its effect on some calcareous soil properties in Khuzestan Province, Iran. Soil samples (n=72) were collected from different regions. To evaluate the effect of carbonates on water contents at pressure head of -1500kpa and PSD of soil samples, these properties were determined before and after removing their calcium carbonate. Based on the results, removal of CaCO3 led to a change in PSD in all the samples and 70% of those changed textural class. Carbonates were most accumulated in clay and sand size in Abadan region while they were accumulated in silt and sand fractions in other areas. Also, evaluation of moisture retention at permanent wilting point (PWP) showed that this feature has been reduced in all samples after removal of carbonates. Following these changes, verification of key to soil taxonomy equation [Clay%= 2.5(% water retained at -1500 kPa tension-%organic carbon)] in calcareous soils of Khuzestan Province showed that this equation can be used with high reliability in calcareous soils of Abadan, Karoon, Haft-Tape agro-industries. However, this equation is not valid in Amir-Kabir and Debal-Khozaiea gro-industries. Our fitted equation [Clay % = (4.35*% water retained at -1500 kPa tension +35.3* % organic carbon)] has high reliability in predicting clay content in non-carbonate samples. This result suggests that the presence of carbonates and its distribution in soil particle size is an important factor in the variability of soil properties at arid and semiarid areas. | ||
| کلیدواژهها | ||
| Keywords:؛ Free carbonate clay؛ Soil taxonomy؛ Water Retention | ||
| مراجع | ||
|
Allison, L. E., & Moodie, C. D. (1965). Carbonates. P. 1379-1396 in: Black (Ed.), Methods of soil Analysis. Part 2, American Society of Agronomy, WI.
Aryanpour, H., Shorafa, M., & Liaghat, A. (2012). Using of pedotransfer functions for studying the effect of soil cultivation on determining of soil moisture at field capacity and permanent wilting point. Journal of Water and Soil, 26, 1042-1050. (In Persian)
Bruand, A., Perez Fernandez, P., & Duval, O. (2003). Use of class pedotransfer functions based on texture and bulk density of clods to generate water retention curves. Soil Use and Management, 19, 232-242.
FAO.UNDP. (1972). Calcareous Soils. Report of the Regional Seminar on Reclamation and Management of Calcareous Soils, 27 Nov., Cairo. Egypt.
Francis, R. E., & Aguilar, R. (1994). Calcium carbonate effects on soil textural class in semiarid Wiland soils. Arid Soil Research and Rehabilitation, 9, 155-165.
Gardner, W. R., Hillel, D., & Benyamini, Y. (1970). Postirrigation movement of soil water: I. Redistribution. Water Resource Research, 6, 851-861.
Gee, G. W., & Bauder, J. W. (1986). Particle size analysis. In: A. Klute (Ed.). Method of soil analysis. Part, 3, 383-411.
Haverkamp, R., & Parlange, J. Y. (1986).Predicting the water retention curve from particle-size, distribution: Sandy soils without organic matter. Soil Science, 142, 325-339.
Hillel, D. (1998). Estimation soil physics. Academic Press, New York.
Jafari, S. (2005). Study of changes in structural, physicochemical, potassium fixation and clay minerals transformation of soils under sugarcane, rotational cropping and non-cultivated soils (Khuzestan), Iran.PhD thesis, Department of Soil Science, Shiraz University, Shiraz. I. R. Iran. 144p.
Jafari, S., & Nadian, H. (2012). Study of a toposequence soil series in some soils of Khozestan province. Journal of water and soil science, 69, 151-163.
Keshavarzi, A., Sarmadian, F., Labbafi, R., & Ahmadi, A. (2011). Developing pedotransfer function for estimating field capacity and permanent wilting point using fuzzy table look-up scheme. Computer and Information Science, 4, 130-141.
Khattab, S. A. A. & Al-Taie. L. Kh. I. (2006). Soil water characteristic curves (SWCC) for lime treated expansive soil from Mosul. Unsaturated Soils, 1671-1682.
Khodaverdiloo, H., & Homaee, M. (2002). Derivation of transfer functions to obtain soil moisture. Journal of Agricultural Engineering, 10 (3), 35-46.
Khodaverdiloo, H., Homaee, M., Van Genuchten, M. T., & Ghorbani, D. S. (2011). Deriving and validating pedotransfer functions for some calcareous soils. Journal of Hydrology, 399, 93–99.
Kishchuk, B. E. (2000). Calcareous soil, their properties and potential limitation of conifer growth in southeastern British Columbia and western Alberta: a literature review. Canadian Forest Service Publications.Inf. Rep. NOR-X-370.
Kroetsch, D., & Wang, C. (2006).Particle size distribution. In: Carter, M.R., Gregorich, E.G. (Eds.), Soil Sampling and Methods of Analysis. CRC Press Taylor and Francis, Boca Raton, FL, pp, 713–725.
Moore, T. J., Hartwing, R. C., &. Loeppert, R. H. (1990). Steady-state procedure for determining the effective particle size distribution of soil carbonates. Soil Science Society of America Journal, 54, 55-59.
Moradi, F. (2012). Estimating the soil moisture retention curve using neural networks - Fuzzy in some Agro-Industries in Khuzestan province. M. Sc. The sis. Department of Soil Science. Ramin University of Agriculture and Natural Resources. Ahvaz. I. R. Iran. 198p.
Motallebi, E., Homaee, M., Zarei, Gh. & Mahmoodi, S. (2011). Studying Effect of Lime on Hydraulic Properties Using Pedotransfer Functions in, Garmsar. Iranian Journal of lrrigation and Drainage, 4, 426-439.
Rajkai, K., Kabos, S., Van Genuchten and, M. Th., & Jansson, P. E. (1996). Estimating of water retention characteristics from the bulk density and particle size distribution of Swedish soils. Soil Science, 161, 832-845.
Rawls, W. J., Pachepsky, Y. A., Ritchie, J. C., Sobecki, T. M., & Blood worth, H. (2003). Effect of soil organic carbon on soil water retention. Geoderma, 116, 61-76.
Sabbah, A., Gorji, M., Rafahi, H., & Shahooe, S. (1999). Relationship between soil erodibility factors (K in USLE) with aggregate stability in major soil series of Qazvin. Iranian Journal of Agriculture Science, 30, 596-609. (In Persian)
Soil survey staff. (2014). Key to soil taxonomy. (12st Ed.). Natural Resources Conservation Service, United States Department of Agriculture.
Zhang, X. C., & Norton, L. D. (2002). Effect of exchangeable Mg on saturated hydraulic conductivity, disaggregation and clay dispersion of disturbed soils. Journal of Hydrology, 260, 194-205. | ||
|
آمار تعداد مشاهده مقاله: 2,536 تعداد دریافت فایل اصل مقاله: 3,384 |
||