تحقیقات علوم زراعی در مناطق خشک

تحقیقات علوم زراعی در مناطق خشک

بیوچار و کاهش اثرات منفی آبیاری با آب شور در خاک‎های زراعی لوم و لوم‎شنی در دشت سیستان

نوع مقاله : مقاله پژوهشی

نویسندگان
1 دانشجوی دکتری گروه مهندسی علوم آب، دانشکده آب و خاک، دانشگاه زابل، زابل، ایران
2 گروه مهندسی علوم آب، دانشکده آب و خاک، دانشگاه زابل، زابل، ایران
3 گروه مهندسی علوم باغبانی و فضای سبز، دانشکده کشاورزی، دانشگاه زابل، زابل، ایران
چکیده
شوری آب آبیاری از مهم‌ترین چالش‌های کشاورزی در مناطق خشک و نیمه‌خشک است. در این پژوهش، اثر بیوچار بر کاهش اثرات مخرب شوری آب آبیاری بر ویژگی‌های فیزیکی و شیمیایی خاک در دو بافت خاک بررسی شد. آزمایش به‌صورت فاکتوریل در قالب طرح بلوک‌های کامل تصادفی و به‌صورت گلدانی در سال 1401 در گلخانه تحقیقاتی دانشگاه زابل انجام شد. تیمارها شامل بافت خاک (لوم و لوم‌شنی)، شوری آب در چهار سطح (0/8، 4، 8 و 12 دسی‌زیمنس بر متر) و بیوچار در چهار سطح (0، 1، 3 و 5 درصد وزنی) بودند. افزایش شوری آب آبیاری هدایت الکتریکی خاک را به‌طور معنی‌داری به‌ویژه در خاک لوم افزایش داد. شوری تأثیر محسوسی بر چگالی ظاهری و pH نداشت، اما موجب افزایش ظرفیت تبادل کاتیونی و سدیم تبادلی شد، درحالی‌که تغییر منیزیم و پتاسیم معنی‌دار نبود. بیوچار سبب کاهش هدایت الکتریکی، چگالی ظاهری و سدیم تبادلی و از طرفی افزایش ظرفیت تبادل کاتیونی و ظرفیت نگهداشت آب شد. کمترین هدایت الکتریکی و چگالی ظاهری در خاک لوم شنی و بیشترین ظرفیت تبادل کاتیونی در خاک لوم مشاهده شد. هدایت هیدرولیکی خاک لوم‌شنی به‌طور معنی‌داری تحت تأثیر شوری و بیوچار قرار گرفت، اما در خاک لوم تغییر قابل‌ملاحظه‌ای نداشت. تیمارهای 3 و 5 درصد بیوچار موجب کاهش سدیم تبادلی و در شوری بالا باعث کاهش منیزیم شدند، ولی پتاسیم تغییر معنی‌داری نداشت. طبق نتایج این پژوهش، بیوچار اصلاح‌کننده‌ای موثر برای بهبود ویژگی‌های خاک و کاهش اثرات نامطلوب شوری آب آبیاری، به‌ویژه در خاک‌های سبک‌تر مانند لوم‌شنی است.
کلیدواژه‌ها

عنوان مقاله English

Biochar mitigates the adverse effects of saline water irrigation on loam and sandy loam agricultural soils in the Sistan plain

نویسندگان English

Ehsan Salari 1
Masoomeh Delbari 2
Abdolrahman Rahimian Boogar 3
Peyman Afrasiab 2
1 Ph.D Student, Department of Water Engineering, Faculty of Water and Soil, University of Zabol, Zabol, Iran
2 Department of Water Engineering, Faculty of Water and Soil, University of Zabol, Zabol, Iran
3 Department of Horticultural Science and Landscape Engineering, Faculty of Agriculture, University of Zabol, Zabol, Iran
چکیده English

Introduction: Soil and water salinity is one of the major environmental and agricultural challenges, particularly in arid and semi-arid regions, leading to reduced soil fertility and crop productivity. Increasing salinity of irrigation water significantly affects the physical and chemical properties of agricultural soils, causing changes and degradation in soil structure. This study aimed to investigate the effect of biochar as a soil amendment on mitigating the adverse impacts of saline irrigation water on the physical and chemical properties of two soil textures: loam and sandy loam, under different salinity levels.
Materials and Methods: A factorial experiment was conducted in a completely randomized block design under greenhouse conditions at the University of Zabol. The experiment included three factors: Soil texture: loam and loamy sand, Irrigation water salinity: at four levels (0.8, 4, 8, and 12 dS/m), and Biochar amendment: at four levels (0%, 1%, 3%, and 5% by volume mixed with the soil). The biochar used in this study was produced from one-year-old grapevine stems, which were crushed, sieved, and mixed with the soil. The measured parameters included electrical conductivity (EC), pH, bulk density, cation exchange capacity (CEC), saturated hydraulic conductivity, and the accumulation of sodium (Na), magnesium (Mg), and potassium (K) in the soil.
Results and Discussion: The results showed that increasing irrigation water salinity significantly raised soil EC, with a more pronounced increase in loam soil compared to sandy loam. Salinity had little effect on bulk density and pH but led to an increase in cation exchange capacity. Although sodium levels rose in both soil textures due to salinity, magnesium and potassium levels remained stable. Applying biochar reduced soil EC, especially in sandy loam, where 3% and 5% biochar treatments caused the greatest reduction, indicating decreased salt buildup due to biochar. Neither saline irrigation nor biochar application significantly changed soil pH in either soil type. However, biochar notably decreased exchangeable sodium at higher salinity levels in both loam and sandy loam soils. Additionally, biochar reduced soil bulk density and enhanced water retention. The greatest decrease in bulk density of the loam texture was observed in treatments with 3% and 5% biochar under irrigation conditions using water with a salinity of 4 dS/m. Additionally, the 1% biochar treatment showed a significant reduction in density under a salinity level of 12 dS/m. The highest decrease in bulk density of the sandy loam texture occurred in the 5% biochar treatment under irrigation with water having salinity levels of 4 and 8 dS/m. Biochar significantly increased soil CEC in both soil types under various salinity levels, with more substantial effects in loam soil. Hydraulic conductivity in sandy loam was significantly affected by both salinity and biochar treatments. Rising irrigation water salinity had different impacts on sodium, magnesium, and potassium accumulation in the two soils. The application of 3% and 5% biochar markedly decreased exchangeable sodium. Magnesium accumulation was higher in loam soil at higher salinity levels, and biochar's effect on magnesium depended on salinity level, biochar amount, and soil type. Notably, at 12 dS/m salinity, 5% biochar significantly reduced magnesium buildup. In contrast, potassium accumulation was unaffected by either salinity or biochar.
Conclusion: Overall, the results of this study indicate that biochar can be considered as an effective soil amendment for improving the physical and chemical properties of soil under saline irrigation conditions. Biochar application can play a vital role in managing soil salinity and enhancing plant tolerance to salinity stress, particularly in lighter-textured soils such as sandy loam.

کلیدواژه‌ها English

Electrical conductivity
Exchangeable sodium
Sandy loam soil
Soil amendment
Soil physico-chemical properties
Water salinity
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  • تاریخ دریافت 05 شهریور 1404
  • تاریخ بازنگری 22 مهر 1404
  • تاریخ پذیرش 25 مهر 1404