نوع مقاله : مقالات پژوهشی
نویسندگان
دانشگاه آزاد اسلامی واحد علوم و تحقیقات فارس
چکیده
در خاک های مناطق خشک و نیمه خشک کمبود مواد آلی یکی از موانع دستیابی به عملکرد مطلوب می باشد. لذا در این پژوهش تأثیر دو نوع ماده آلی بر برخی ویژگی های فیزیکی خاک بررسی گردید. آزمایش به صورت فاکتوریل در قالب طرح کاملاً تصادفی، شامل دو منبع ماده آلی کمپوست و ضایعات میوه رسیده انجیر هر کدام در چهار سطح (0، 1، 2 و 4 درصد وزنی) و سه نوع بافت خاک (شن لومی، لوم و لوم رسی سیلتی) در سه تکرار انجام گرفت. خصوصیات فیزیکی خاک شامل چگالی ظاهری، چگالی حقیقی، تخلخل، درصد اشباع رطوبتی و مقاومت فروروی سله ی خاک اندازه گیری شدند. نتایج نشان داد که کاربرد ضایعات میوه رسیده انجیر و کمپوست در خاک باعث افزایش معنی دار درصد اشباع رطوبتی و کاهش معنی دار مقاومت فروروی سله خاک در مقایسه با تیمار شاهد گردید. کاربرد ضایعات میوه رسیده انجیر و کمپوست باعث افزایش تخلخل خاک و کاهش جرم مخصوص ظاهری و جرم مخصوص حقیقی خاک در مقایسه با تیمار شاهد گردید. ولی این افزایش و کاهش معنی دار نبود. کاهش مقاومت فروروی سله خاک در نتیجه کاربرد ضایعات میوه رسیده انجیر بیشتر از کمپوست بود در حالی که کاربرد کمپوست در خاک در مقایسه با ضایعات میوه رسیده انجیر تأثیر بیشتری بر روی چگالی ظاهری، چگالی حقیقی، تخلخل و درصد اشباع خاک داشت. نتایج نشان داد که کاربرد این دو منبع ماده آلی سبب بهبود ویژگی های فیزیکی اندازه گیری شده در خاک، شامل مقاومت فروروی سله ی خاک، چگالی ظاهری، چگالی حقیقی، تخلخل و درصد اشباع رطوبتی خاک شد.
کلیدواژه‌ها
عنوان مقاله [English]
The Effect of Compost and the Ripe Fruit Waste of Fig on some Physical Properties of Surface Soil
نویسندگان [English]
- zahra dianat maharluei
- ali akbar moosavi
Islamic Azad University, Fars
چکیده [English]
Introduction: In arid and semi-arid soils, low organic matter is one of the barriers to achieving optimal performance. The soils with more organic matter have a better structure and are more resistant to erosive factors such as water and wind. Soil organic matter has a particular importance and has significant impact on the stability of soil aggregates, the extension of plant root system, carbon and water cycles and soil resistance to erosion. This substance acts as a cementing agent and plays an important role in soil flocculation and formation of resistant aggregates.Also, the addition of organic matter to the soil increases soil porosity and decreases soil bulk density.
Materials and Methods: In this research, the effect of the two types of organic matter (compost and the ripe fruit waste of fig) on some soil physical properties was studied. A factorial experiment based on completely randomized design, including the four levels of compost and the ripe fruit waste of fig (0, 1, 2 and 4 by weight %) and three soil types (loamy sand, loam and silty clay loam) with three replications was carried out. The soil samples were collected from the three territories of Fars Province: loamy sand soil from Shiraz, loamy soil from Maharlu and Silty clay loam soil from Zarghan area. The soil samples were air dried and passed through a 2 mm sieve. The physical properties including the bulk density, particle density, porosity, moisture content and soil crust strength was measured. In this research, the soil texture by hydrometer method, Electrical conductivity of the soil saturated paste extract by electrical conductivity meter, saturated paste pH by pH meter, seedling emergence test, soil crust strength by a pocket penetrometer (HUMBOLDT MFG.CO.) bulk density by cylindrical sample and particle density by pycnometer method were measured. The fig fruit treatments were prepared by thoroughly mixing the dried powder of ripe fig fruit passed through a 2 mm sieve (with the rates of 0, 1, 2, and 4 % by dry weight) with the air dried soils. Also, the compost treatments were prepared by thoroughly mixing the dried powder of compost passed through a 2 mm sieve (with the rates of 0, 1, 2, and 4 % by dry weight) with the air dried soils. The test measurement PVC cylinders with an inner diameter of 12.5 cm and a height of 20 cm were prepared. The bottom ends of the cylinders were closed with a screened PVC plate. These cylinders were uniformly filled with the treated soils and irrigated a few times to make a homogeneous soil column. About 3 cm of the top end of the cylinders were left empty.
Results and Discussion: The results showed that all the rates of the ripe fruit waste of fig and the compost treatments significantly decreased crust strength of all soils compared to control at 1% probability level. The results also showed nearly the greater effect of all the treatments on crust strength of loamy sand soil compared to the other soils. All the rates of the ripe fruit waste of fig and compost treatments significantly increased the moisture content of all the soils compared to control at 1% probability level. Moreover, the greater effect of all the treatments on the moisture content of silty clay loam soil compared to other soils was generally observed. All the rates of the ripe fruit waste of fig and compost treatments decreased the bulk density and particle density of all the soils compared to control. Tthe greatest impact was observed in the compost treatments at the level of 4% by dry weight and silty clay loam texture. Also, all the rates of the ripe fruit waste of fig and compost treatments increased the porosity of all the soils compared to control, and the greatest impact belonged to the compost treatments at the level of 4% by dry weight andsilty clay loam texture.
Conclusion: The results showed that the use of the ripe fruit waste of fig and compost in the soil increased moisture content and decreased crust strength significantly compared to the control. Also, the ripe fruit waste of fis and compost in the soil increased porosity and decreased bulk density and particle density compared to the control, but this increase and decrease were not significant.Reduction in crust strength caused by the ripe fruit waste of fig application was more than compost application. However, the effect of compost application on the soil bulk density, particle density, porosity and moisture content was more than the ripe fruit waste of fig application.
کلیدواژه‌ها [English]
- Bulk density
- Crust Strength
- porosity
- Soil texture
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