بررسی اثر حاصلخیزی و بافت خاک بر تبخیر- تعرق و ضریب گیاهی ذرت علوفه‌ای

نوع مقاله : مقالات پژوهشی

نویسندگان

پردیس کشاورزی و منابع طبیعی کرج

چکیده

در این تحقیق اثر حاصلخیزی و بافت خاک بر ضریب گیاهی و تبخیر- تعرق گیاه ذرت بررسی گردید. آزمایش به صورت فاکتوریل در قالب طرح کاملاً تصادفی با سه تیمار بافت خاک شامل لوم رسی سیلتی، لوم و لوم شنی و سه تیمار حاصلخیزی خاک، در سه تکرار در مزرعه آزمایشی در بخش جی و قهاب شهرستان اصفهان به اجرا در آمد. به منظور تعیین تبخیر- تعرق گیاه مرجع از روش تشت تبخیر و جهت تعیین تبخیر- تعرق واقعی از روش بیلان حجمی آب خاک با استفاده از میکرولایسیمتر زهکش‌دار استفاده گردید. نتایج بدست آمده نشان داد که با افزایش حاصلخیزی خاک تبخیر- تعرق و ضریب گیاهی ذرت افزایش یافت. بیشترین میانگین ده روزه تبخیر- تعرق ذرت در دهه پنجم رشد در خاک لوم رسی سیلتی با افزودن دو درصد کود برابر با 76/8 میلی‌متر بر روز بدست آمد که از کمترین میانگین ده روزه تبخیر- تعرق ذرت در این دهه 5/45 درصد بیشتر شد. ضریب گیاهی ذرت در مرحله میانی رشد بیشتر از مراحل دیگر تحت تاثیر تیمارهای متفاوت حاصلخیزی خاک قرار گرفت. بیشترین و کمترین تاثیر افزایش حاصلخیزی خاک بر افزایش ضریب گیاهی ذرت در مرحله میانی رشد به ترتیب 8/37 درصد در خاک لوم با افزودن دو درصد کود و 3/18 درصد در خاک لوم شنی با افزودن دو درصد کود بدست آمد.

کلیدواژه‌ها


عنوان مقاله [English]

Investigating the Effect of Soil Texture and Fertility on Evapotranspiration and Crop Coefficient of Maize Forage

نویسندگان [English]

  • M. Ghorbanian Kerdabadi
  • Hamideh Noory
  • A.M. Liaghat
University of Tehran
چکیده [English]

Introduction: Crop coefficient varies in different environmental conditions, such as deficit irrigation, salinity and intercropping. The effect of soil fertility and texture of crop coefficient and evapotranspiration of maize was investigated in this study. Low soil fertility and food shortages as a stressful environment for plants that makes it different evapotranspiration rates of evapotranspiration calculation is based on the FAO publication 56. Razzaghi et al. (2012) investigate the effect of soil type and soil-drying during the seed-filling phase on N-uptake, yield and water use, a Danish-bred cultivar (CV. Titicaca) was grown in field lysimeters with sand, sandy loam and sandy clay loam soil. Zhang et al (2014) were investigated the Effect of adding different amounts of nitrogen during three years (from 2010 to 2012) on water use efficiency and crop evapotranspiration two varieties of winter wheat. The results of their study showed. The results indicated the following: (1) in this dry land farming system, increased N fertilization could raise wheat yield, and the drought-tolerant Changhan No. 58 showed a yield advantage in drought environments with high N fertilizer rates; (2) N application affected water consumption in different soil layers, and promoted wheat absorbing deeper soil water and so increased utilization of soil water; and (3) comprehensive consideration of yield and WUE of wheat indicated that the N rate of 270 kg/ha for Changhan No. 58 was better to avoid the risk of reduced production reduction due to lack of precipitation; however, under conditions of better soil moisture, the N rate of 180 kg/ha was more economic.
Materials and Methods: The study was a factorial experiment in a completely randomized design with three soil texture treatment, including silty clay loam, loam and sandy-loam soil and three fertility treatment, including without fertilizer, one and two percent fertilizer( It was conducted at the experimental farm in Jey and Qahab district of Isfahan. Reference evapotranspiration and actual evapotranspiration of maize were measured by evaporation pan method and volumetric soil water balance method using micro lysimeters, respectively. In order to accommodate the growing field conditions, a ditch with a depth of 25 cm, length of 240 cm and width of 300 cm were dug and micro-lysimeters were placed it in three rows (three replications) with a distance of 75 cm. After preparing the treatments, four seed Maize with variety of NS540 were planted at a depth of 3-5 cm on 5 August. To reduce the oasis effect on evapotranspiration, the same corn was planted in the vicinity of the project area with 500 square meters..
Results and Discussion: The results showed that using fertilizer caused increasing of crop evapotranspiration and crop coefficient of maize. Maximum of the ten-day average evapotranspiration of maize in the silty clay loam soil with two percent fertilizer was obtained 8.76 (mm/ day) on the fifth decade of growth and this value was found 45.5 percent higher than the lowest mean evapotranspiration value of the ten-day. Comparison evapotranspiration of maize in different soil fertility treatments showed that the greatest impact on increasing of maize evapotranspiration in SLF2, SCLF2, SLF2 treatments were obtained that was equal %19.1, %14.3 and %10.6, respectively (table 4). Most of the effects of fertility the crop coefficient of maize at the middle stage of growth was influenced more than other stages by the different treatments of soil fertility. Adding one and two percent of the fertilizer to treatment SCLF0 increased maize crop coefficient about 3.5 and 9.7 percent at development stage, respectively, That measured %6 and 11% for LF1 and LF2 treatments, respectively, and about 1.6 and 5.6% for SLF2 SLF1 treatment, respectively (Table 6). Comparison of maize middle crop coefficient in SLF2 and SLF1 for different soil fertility treatments showed that effect of increasing soil fertility on middle Kc of maize was more than other stages of plant growth (Table 6). The obtained results showed that the addition of one and two percent fertilizer to the silty clay loam soil increased, the middle crop coefficient 13.3% and 27%, respectively in.
Conclusion: Maximum and minimum effect of soil fertility on increasing crop coefficient of maize in the middle stage was equal to 37.8% in the loamy soil and 18.3% in the sandy loam soil with two percent fertilizer. The greatest effect of soil fertility on crop coefficient of maize was measured 8.37% in the middle stage of growth in LF2. The effect of soil fertility on crop coefficient of maize in loam and silty clay loam soils more than sandy loam soil, Because can be a further organic matter in these soils (loam and silty clay loam and also decreasing evaporation in sandy loam soil.

کلیدواژه‌ها [English]

  • Fertilizer
  • Growth Stages of Maize
  • Soil Type
  • water requirement
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