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The effect of irrigation with magnetized water of varying salinity on some chemical properties of the soil and leachate of Kaskeis area (Aleppo governorate)

أثر الري بمياه ممغنطة متباينة الملوحة في بعض الخواص الكيميائية لتربة وراشح منطقة كصكيص (محافظة حلب)

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 Publication date 2023
and research's language is العربية
 Created by د. يوسف الخلف




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A column experiment was carried out under the conditions of the laboratory of colloids and clay minerals at the Faculty of Agricultural Engineering at the University of Aleppo, in order to know the effect caused by the magnetization of irrigation water on the chemical properties of soils irrigated with water of different salinity. The experiment was carried out on the Kskeis soil, located east of Aleppo city, and it was irrigated with three types of water of different salinity (Furat - Rasm Al-Hamis - Mishrifat Al-Zakiya). With irrigated water, the irrigation process was carried out with ten irrigations. The results indicated that the magnetization of showing off water reached its value, reached its value, reached its value, reached its value when magnetized. dS.m-1) was 4.05, while at the non-magnetized (dS.m-1) 3.7, the values of the sorbent sodium rate SAR were affected by the accumulation of salts in the subsurface layer of the studied treatments included in the study. The values of the rate of sodium adsorption SAR were also affected by the accumulation of salts in the subsurface layer of the studied treatments included in the study, and the magnetization of water contributed to the reduction of SAR values. 1.57, while it reached 1.93 in the same treatment irrigated with non-magnetized water.


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Research summary
أجريت تجربة أعمدة في مختبر الغرويات ومعادن الطين في كلية الهندسة الزراعية بجامعة حلب، لدراسة تأثير مغنطة مياه الري على الخواص الكيميائية للتربة المروية بمياه مختلفة الملوحة. تم استخدام تربة من منطقة كصكيص شرق حلب، وريها بثلاثة أنواع من المياه ذات ملوحة مختلفة (مياه الفرات، مياه بئر رسم الحميس، ومياه بئر مشرفة الزكية). تم تطبيق تقنية الري بمياه ممغنطة وغير ممغنطة مع معامل غسيل بنسبة 15%، وتمت عملية الري بعشر ريات. أظهرت النتائج أن مغنطة مياه الري ساهمت في تخفيض قيم الملوحة في التربة مقارنة بالمياه غير الممغنطة، كما ساهمت في تخفيض قيم معدل الصوديوم المدمص (SAR). تم تحليل الراشح من التربة المروية وأظهرت النتائج أن مغنطة المياه أدت إلى تحسين كفاءة غسل الأملاح من التربة. تشير النتائج إلى أن استخدام المياه الممغنطة يمكن أن يكون له تأثير إيجابي على تحسين جودة التربة وتقليل تراكم الأملاح فيها، مما يعزز من كفاءة استخدام المياه في الزراعة في المناطق الجافة وشبه الجافة.
Critical review
دراسة نقدية: تعتبر هذه الدراسة خطوة هامة في مجال تحسين جودة التربة باستخدام تقنيات غير تقليدية مثل مغنطة المياه. ومع ذلك، هناك بعض النقاط التي يمكن تحسينها في الدراسات المستقبلية. أولاً، يجب إجراء تجارب ميدانية على نطاق أوسع للتحقق من نتائج التجارب المخبرية. ثانياً، يجب دراسة تأثير مغنطة المياه على أنواع مختلفة من التربة والمحاصيل الزراعية لضمان تعميم النتائج. ثالثاً، يمكن أن تكون هناك حاجة لدراسة تأثير مغنطة المياه على المدى الطويل لضمان عدم حدوث تأثيرات سلبية غير متوقعة. وأخيراً، يجب النظر في التكلفة الاقتصادية لتطبيق هذه التقنية على نطاق واسع ومدى جدواها الاقتصادية مقارنة بالطرق التقليدية.
Questions related to the research
  1. ما هو الهدف الرئيسي من هذه الدراسة؟

    الهدف الرئيسي من الدراسة هو معرفة الأثر الذي يسببه الماء الممغنط في الخواص الكيميائية للترب المروية بمياه متباينة الملوحة، وذلك من خلال دراسة تأثير الري بالمياه المالحة الممغنطة وغير الممغنطة في قيم التوصيل الكهربائي ومعدل الصوديوم المدمص للتربة والراشح في منطقة كصكيص.

  2. ما هي أنواع المياه المستخدمة في التجربة؟

    تم استخدام ثلاثة أنواع من المياه ذات ملوحة مختلفة في التجربة: مياه الفرات، مياه بئر رسم الحميس، ومياه بئر مشرفة الزكية.

  3. ما هو تأثير مغنطة المياه على قيم التوصيل الكهربائي للتربة؟

    أظهرت النتائج أن مغنطة مياه الري ساهمت في تخفيض قيم التوصيل الكهربائي للتربة مقارنة بالمياه غير الممغنطة، مما يشير إلى تحسين كفاءة غسل الأملاح من التربة.

  4. كيف أثرت مغنطة المياه على معدل الصوديوم المدمص (SAR) في التربة؟

    ساهمت مغنطة المياه في تخفيض قيم معدل الصوديوم المدمص (SAR) في التربة، حيث كانت قيم الصوديوم المدمص أقل في التربة المروية بمياه ممغنطة مقارنة بالتربة المروية بمياه غير ممغنطة.


References used
6- كاظم، رعد جواد محمد (2010). استخدام المياه الممغنطة في استصلاح الترب المتأثرة بالأملاح. مجلة الفرات للعلوم الزراعية 2-(2). 97-103.
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A column experiment was carried out under the conditions of the laboratory of colloids and clay minerals at the Faculty of Agricultural Engineering at the University of Aleppo. The aim of study is know the effect caused by the magnetization of irriga tion water on the physicochemical properties of soils irrigated with water of different salinity. The experiment was carried out on selected gypsiferous soils from the village of Musharafa Al-Zakiya located in the Maskana project (Aleppo governorate). And it was irrigated with three types of water of different salinity (Euphrates River water -Rasm Al-Hamis village - Musharafa Al-Zakiya village). Irrigation technology was applied With magnetized water (M) and water without magnetization (NM), a leaching factor of 15% was used with water added to the columns, and the irrigation process was repeated ten times. The results indicated that the use of the water of Rasm Al-Hamis well and the well of Mishrifa, the magnetic purity, contributed to the washing of salts by 20% and 16% for the surface and subsurface layers, respectively, compared to similar treatments irrigated with normal water, and the results of the statistical analysis indicated that the decrease in the concentration of salts in the washed columns The magnetized water was significant. As for the magnetized water of the Euphrates, it contributed to the washing of salts from the surface layer within the soil columns by about 5.5%, compared with the treatment irrigated with non-magnetized Euphrates river water, and the decrease in the concentration of salts was not significant. The data indicated in general to the significant role of the washing coefficient applied in this study in the disposal of salts, in particular soda salts, as the data showed that the magnetization of water added to the studied soil columns contributed clearly in reducing the values of the adsorbed sodium ratio (SAR) and the ratio of exchangeable sodium (ESP) compared to the non-magnetized irrigation water. The magnetization of water also contributed to improving the porosity of soil irrigated with magnetized water, compared to treatments irrigated with ordinary water.
The pot experiments were carried out under the conditions of the glass house at the Faculty of Agriculture, University of Aleppo. The aim of the present study is to determine the role of gypsum and humic acid on some chemical properties of irrigated soil by saline water. The experiment was designed in a split second-order manner, with the main sections containing three levels of salinity irrigation water using sodium chloride salt as (W1:0, W2:3, W3:6 g𝓁-1). Three levels of gypsum were mixed: as (G1:0 , G2:25, G3:50 g). Three levels of acids were added with irrigation water as (H1:0,H2:24, H3:48 kg/he). The experiments for application leaching factor with irrigation water were carried out for treatment (W2,W3) at two levels as (%10 and %20) of field capacity, respectively. The results showed that the salt accumulation was higher when applied the leaching factor (W2), while the salt accumulation was decreased when the wash factor (W3) was applied. The addition of gypsum levels contributed for increasing in EC values, especially in the surface layer. The role of humic acid was effectively demonstrated in saline soils (W3, W2), where the concentration of sodium ions, SAR and ESP were significantly reduced when applying a high level of humic acid with irrigation water. The SAR values and the sodium-sodium ratio (ESP) were affected by the accumulation of salts in the surface layer.
The effect of clay soil treatment with two levels of tobacco west compost and organic fertilizer (15 and 30 ton/ h), in addition to mineral fertilizer treatment, with three replicates of each treatment on some physical properties (Aggregate size di stribution, main weight diameter, bulk density and porosity) and chemical properties (Organic carbon, humic and volvic acid and humification index for big and small soil aggregates was studied. The results showed that tobacco west compost and organic fertilizer were effective in increment of soil content of organic carbon, which reached (20 and 26%) for organic fertilizer, and (39 and 45%) for compost compared to the control, conducing to ameliorate soil physical properties, where The main weight diameter, stable aggregate rate and soil porosity were increased. Whereas, bulk density decreased significantly in both treatments compared to the control. Compost treatment affect soil physical properties more than organic fertilizer.Mineral fertilizer decreased soil content of organic carbon compared to the control. Humic and volvic acids contents were between 2.12 and 74.3 mg/kg aggregates in the control,and compost treatments alternatively in macro aggregates (> 2mm). Wile, volvic acid values were between 0.93 mg/kg in control for small aggregates (< 0.25), and 3.17 mg/kg aggregates in mineral fertilizer treatment for (0.25 – 2) aggregates. Humification index values were less than 2 in macro aggregates, while it was bigger than 2 in small aggregates.
The research was conducted in order to study the effect of irrigation with sulfuric saline water on some major soil properties and maize production The flood irrigation process was carried out with four treatments: Treatment of witness was irrigated with fresh water, treatment No. (1) was irrigated with sulfuric saline water according to the standardized maize irrigation, and treatment No. (2) was also irrigated with salty sulfur water standardized for maize irrigation + 20% washing rate, and treatment No. (3) was irrigated with water Sulfur saline according to maize irrigation standard + 30% washing rate,The results of the study showed that there was a slight significant difference between the four treatments in terms of the apparent and real density, while there were clear significant differences between the treatments in terms of ESP%, EC and carbonates with depth, and this was the result of washing salts with the excess amount of irrigation water used for washing. The results also show that treatment No. (3) was the best of germination percentage and productivity, while treatment No. (1) achieved the lowest germination and productivity(Fresh maize cobs yield with wrappers) , as the readings were as follows: The percentage of germination in the witness was 95%, in treatment (1) 90%, and in treatment (2) 95% and in treatment (3) 97%, while the productivity was in the witness 32.4 tons / ha and in treatment (1) 30.25 tons / ha and in treatment (2) 33.6 tons / ha and in treatment (3) 39.037 tons / ha. This indicates that irrigation with sulfuric saline water according to (water ration for maize + 30% washing) achieved the best results, as the economic feasibility of using sulfuric saline water was achieved by obtaining good production, providing fresh water and preserving the major properties of the soil.
A laboratory experiment was carried out in the Clay Minerals and Colloids Laboratory in the Department of Soil Sciences and Land Reclamation at the Faculty of Agricultural Engineering - University of Aleppo. The research aims to know the effect of tw o types of salts (NaCl - Na2SO4) with five concentrations of each of the salts studied in the laboratory experiment on the stability of artificial soil aggregates and to know the salt concentrations that cause the greatest damage in the destruction of artificial soil aggregates. The results indicated the effect of the increased concentration of salts in increasing the percentage of aggregates that were subjected to collapse. The study also indicated that soil aggregates were damaged more by sodium chloride salt compared to sodium sulfate salt. The results indicated that sodium chloride salt contributes to the destruction of soil aggregates, especially at a concentration of 10 g.𝓁-1, where the percentage of destroyed aggregates reached about 35%. Sodium sulfate salt also contributed to the destruction of soil aggregates, and the highest value for the percentage of destroyed aggregates was (25.1%) at a concentration of 8 g.𝓁-1.

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