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تأثیر کاربرد مواد آلی بر برخی ویژگی های فیزیکی خاک در شرایط شور | ||
| پژوهش های آبخیزداری | ||
| مقاله 8، دوره 33، شماره 3 - شماره پیاپی 128، مهر 1399، صفحه 108-121 اصل مقاله (751.87 K) | ||
| نوع مقاله: پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22092/wmej.2019.127741.1259 | ||
| نویسندگان | ||
| سید علی محمد چراغی* 1؛ محمد جواد روستا2؛ شاهرخ شجری3 | ||
| 1استادیار پژوهشی بخش تحقیقات حفاظت خاک و آبخیزداری، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان فارس، سازمان تحقیقات، آموزش و ترویج کشاوزی، شیراز، ایران | ||
| 2دانشیار پژوهشی بخش تحقیقات حفاظت خاک و آبخیزداری، مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان فارس، سازمان تحقیقات، آموزش و ترویج کشاوزی، شیراز، ایران | ||
| 3استادیار پژوهشی دفتر امور اقتصادی، سازمان تحقیقات،آموزش و ترویج کشاورزی، تهران، ایران | ||
| چکیده | ||
| شور و سدیمی‌شدن خاک از عامل‌های مهم تخریب زمین بهویژه در منطقه‌های خشک و نیمهخشک است که اگر به آن توجه نشود منجر به فرسایش میشود و تهدیدی برای پایداری خاک در عرصههای مختلف آبخیزها است. در این پژوهش، تأثیر کاربرد مواد آلی بر برخی ویژگی‌های فیزیکی خاک در شرایط آبیاری با شوری‌های مختلف آب به‌روش فاکتوریل در قالب طرح آماری کاملاٌ تصادفی در سه تکرار به مدت یک سال بررسی شد. عاملها دو سطح شوری آب آبیاری با هدایت الکتریکی 7 و 14 دسیزیمنس بر متر، دو بافت خاک شنی-میانه‌بافت (لومی) و رسی-میانه‌بافت و چهار نوع مادهی آلی شامل ضایعات شیرینبیان، لیموترش، کود مرغی و کود گوسفندی بود. نتایج نشان داد که مواد آلی تأثیر معنی‌داری بر حفظ رطوبت و کاهش تبخیر از سطح خاک (01/0p <) و کاهش جرم مخصوص ظاهری خاک (05/0p <) داشت. درصدرطوبت وزنی خاک با بافت شنی-میانه‌بافت در تیمارهای مواد آلی به‌ترتیب 25، 20، 15 و 15% نسبت به تیمار شاهد افزایش یافت. بین تیمارهای بررسی‌شده، کم‌ترین تبخیر از ستون خاک در تیمار شیرینبیان بود (39/99 سانتیمتر) که نسبت به مقدار آن از سطح خاک در تیمارشاهد (43/26 سانتیمتر)، 8% کاهش نشان داد (0/05p <، آزمون دانکن). نتیجه‌ها نشان‌دهنده‌ی تأثیر معنیدار بافت خاک بر مقدار رطوبت در عمق ستون خاک بود (0/01p <). از آن‌جا که نقش تیمار شیرینبیان در کاهش‌دادن تبخیر از طح و حفظ رطوبت خاک برجسته بود، پیشنهاد میشود بررسیهای تکمیلی برای بررسی امکان کاربرد این نتیجه‌ها در برنامههای حفاظت آب و خاک، بهویژه در زمین شیبدار انجام شود. | ||
| کلیدواژه‌ها | ||
| تبخیر؛ رطوبت وزنی؛ شیرین بیان؛ کود دامی | ||
| عنوان مقاله [English] | ||
| Effect of Organic Matter Application on some Soil Physical Properties under Saline Conditions | ||
| نویسندگان [English] | ||
| Seyed Ali Mohammad Cheraghi1؛ Mohammad Javad Rousta2؛ Shahrokh Shajari3 | ||
| 1Assistant Prof. Soil Conservation and Watershed Management Research Department, Agricultural and Natural Resources Research and Education Center of Fars Province, Agricultural Research, Education and Extension Organization, Shiraz, Iran | ||
| 2Associate Prof. Soil Conservation and Watershed Management Research Department, Agriculture and Natural Resources Research and Education Center of Fars Province, Agricultural Research, Education and Extension Organization, Shiraz, Iran | ||
| 3Assistant Prof. Office of Economic Affairs, Agricultural Research, Education and Extension Organization, Tehran, Iran | ||
| چکیده [English] | ||
| Soil salinization and sodification are important factors in soil degradation, especially in arid and semi-arid regions, which, if not considered, can lead to erosion that threatens soil stability in different regions of watersheds. Effects of organic matter application on some soil physical properties under irrigation with saline waters was investigated. The experiment was conducted as factorial based on complete randomized design with three replications for a period of one year. Treatments included two levels of irrigation water salinities of 7 and 14 dS/m, two soil textures, namely sandy loam and clay loam, and four sources of organic matters, namely licorice and lemon dregs and chicken and sheep manure. Results showed that organic matter had a significant effect on moisture retention and evaporation from the soil surface (P <0.01) and reduction of soil bulk density (p < 0.05). The percent moisture content of the loamy sandy soils treated with licorice and lemon dregs and chicken and sheep manure increased by 25, 20, 15 and 15%, respectively. The lowest evaporation from the soil columns occurred in licorice treatment amounting to 39.99 cm, which was 8% lower compared to evaporation from the control treatment (43.26 cm). This decrease was statistically significant at the 5% level with the Duncan's test. The results also showed a significant effect of soil texture on soil moisture content at lower depths (P <0.01). Regarding the prominent role of licorice treatment in reducing evaporation from the surface and maintaining soil moisture, further studies are suggested on the feasibility of applying the results in soil and water conservation programs, especially on sloping lands. | ||
| کلیدواژه‌ها [English] | ||
| Evaporation, licorice, manure, moisture content by weight | ||
| مراجع | ||
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Alimardani A, Delaver MA, Golchin A. 2011. The effect of organic and inorganic materials on some physical properties of a sodic soil. Journal of Soil Management and Sustainable Production. 1(2):21–37. Amooh MK, Bonsu M. 2015. Effects of soil texture and organic matter on evaporative losses of soil moisture. JOGAE. 3(3): 152–161. Asadi Kapourchal S, Homaee M. 2017. Using desalinization models for scheduling crop rotation of saline-sodic soils: a case study in Ramhormoz region, Iran. Water and Soil Conservation Journal. 6(4): 92–106. Banie MH. 2001. Soil map of IRAN: Land resources and potentialities. Tehran, Iran: Soil and Water Research Institute. Baohia GU, Harvey ED. 1993. Disperisions and aggregation of soils as influenced by organic and inorganic polymers. Soil. Sci. Soc. Am. 57(3): 709–716. Barzegar AR, Nelson NP, Malcolmoades J, Rengasamy P. 1997. Organic matter, sodicity, and clay type: Infuence on soil aggregation. Soil. Sci. Soc. Am. J. 61(4): 1131–1137 Bauer A, Black AL. 1981. Soil carbon, nitrogen, and bulk density comparisons in two cropland tillage systems after 25 years and in virgin grassland. Soil Sci. Soc. Am. J. 45(6): 1166–1170. Celik I, Ortas I, Kilic S. 2004. Effects of compost, mycorrhiza, manure and fertilizer on some physical properties of a chromoxerert soil. Soil and Tillage Research. 78(1): 59–67. Dawish OH, Persaud N, Martens DC. 1995. Effect of long-term application of animal manure on physical properties of three soils. Plant Soil. 176: 289–295. Ding Y, Huang H, Wang L, Zhang Z, Zhang W. 2014. Effect of different organic matter content on soil moisture dynamics, Applied Mechanics and Materials. pp. 481–484. Emami H, Astaraei AR. 2012. Effect of organic and inorganic amendments on parameters of water retension curve, bulk density and aggregate diameter of a saline-sodic soil. pp. 1625–1636. FAO 2005. The importance of soil organic matter. FAO Soils Bulletin No.80. Rome. 78 p. Gill BS, Jalota S K.1996. Evaporation from soil in relation to residue rate, mixing depth, soil texture and evaporativity. Soil Technol. 8(4): 293–301. Graham CB. 2004, Evaporation from bare soil and soil cracks, a thesis submitted to oregon state university in partial fulfillment of the requirements for the degree of master of science. 54 p. Hank JR. 1992. Applied soil physics, Second edition, Springer-Verlog. 176 p. Hudson, B D. 1994. Soil organic-matter and available water capacity. Journal of Soil and Water Conservation. 49 (2):189–194. Khaleel, R, Reddy, KR, and Overcash, MR. 1981. Changes in soil physical properties due to organic waste applications: A review. J. Environ. Qual. 10(2):133–141. Lal R, Stewart BA, Eds. 2012. Soil water and agronomic productivity (advances in soil science), CRC Press, Taylor & Francis Group, New York. pp. 427–454. Lal R. 2009. Soil quality impacts of residue removal for bioethanol production. Soil & Tillage Research. 102 (2):233–241. Rahman HA, Dahab MH, Mustafa, MA. 1996. Impact of soil amendements on intermittent evaporation, moisture distribution and salt redistridation in saline-sodic clay soil colums. Soil. Sci. 161(11): 793–802. Rawls WJ, PachepskyYA, Ritchie JC, Sobecki TM, Bloodworth H. 2003. Effect of soil organic carbon on soil water retention. Geoderma. 116 (1–2):61–76. Rousta MJ, Golchin A, Siadat H. 2001. The effect of organic matter and mineral calcium compounds on aggregate size distribution and dispersible clay in a sodic soil. Soil and Water Sciences Journal. 15(2): 242–260. (In Persian). Rousta MJ, Golchin A,Siadat H, Saleh Rastin N. 2002. Effects of organic matter and mineral compounds on some chemical properties and biological activity of a sodic soil. Soil and Water Sciences Journal. 16(1): 33–45. (in Persian) Rousta MJ, Enayati K. 2013. Effects of organic and mineral amendments on mean-weight diameter of soil aggregates. Watershed Management Research. Pajouhesh & Sazandegi. 98(1): 24–33. (In Persian). Sommerfeldt TG, Chang C. 1985. Changes in soil properties under annual applications of feedlot manure and different tillage practices. Soil Sci. Soc. Am. J. 49(4): 983–987. Szabolcs I. 1994. Soils and salinization. p. 3–11. In M. Pessarakli (ed.) HB of plant and crop stress. Marcel Dekker, New York. 160 p. Tisdale JM, Oades JM. 1982. Organic matter and water-stable aggregates in soils. Journal of Soil Science. 33(2):141–163. Wuest SB, Caesar-TonThat TC, Wright SF, Williams JD. 2005. Organic matter addition, N, and residue burning effects on infiltration, biological, and physical properties of an intensively tilled silt-loam soil. Soil & Tillage Research. 84 (2):154–167. Wythers KR, Lauenroth WK, Paruelo JM. 1999. Bare-Soil Evaporation under semiarid field conditions. Soil Sci. Soc. Am. J. 63(5):1341–1349. Zhang H, Hartge KH, Ringe H. 1997. Effectiveness of organic matter incorporation in reducing soil compacitibility. Soil Sci. Soc. Am. J. 61(1): 239–254. | ||
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