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azerbaijannewsgazette · 2 months
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President Ilham Aliyev presented Garabagh horse to his Kyrgyz counterpart
http://dlvr.it/T63l21
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thebusinesspress · 7 months
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New Era of Regional Integration in the South Caucasus
The recent events in the South Caucasus region have marked a significant turning point in the long-standing conflict between Armenia and Azerbaijan. In the wake of the collapse of the separatist regime in the Garabagh region of Azerbaijan, there are newfound prospects for mutual recognition of territorial integrity and regional integration. These developments have set the stage for a more stable…
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metbuat · 2 years
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The head coach of "Olympiakos" SPOKE about the upcoming game with "Qarabag".
The head coach of “Olympiakos” SPOKE about the upcoming game with “Qarabag”.
We want to win against “Karabakh”. We can do it.” According to “Report”, the head coach of “Olympiakos” Michel Gonzalez said this at a press conference before the third round match of the UEFA Europa League group stage, which they will play against “Garabagh” in Greece. The Spanish specialist said that he has no other thoughts than winning 3 points: “We know well which team we represent. My game…
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yalaninfo · 3 years
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Şuşa Fatehi Hikmət Mirzəyev 🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿🇦🇿 #HimətMirzəyev #HikmetMirzeyev #HikmatMirzayev #Şuşa #Shusha #Susa #Qarabağ #Garabagh #Karabakh #FreeKarabakh #FreeShusha #8Noyabr #ZəfərGünü #ZeferGunu #ZaferGünü #Azerbaycan #Azərbaycan #Azerbaijan #ŞuşaQarabağ #YALANinfo @YALAN.info www.YALAN.info (at Shusha Azerbaijan) https://www.instagram.com/p/CV_WHWdo2HF/?utm_medium=tumblr
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skysfullofrainbow · 4 years
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nazmiyalantiquerugs · 6 years
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Could early collectible rug like this early 18th century Karabagh become a decorative rug? . . . . . #karabagh #garabagh #earlyrugs #18thcenturyrug #caucasianrugs #collectables #decorativerugs #luxuryhomes #interiordesign #interiordesigners #antiquerugs #rareandbeautiful #nazmiyalcollection https://www.instagram.com/p/BqSyIbCgpla/?utm_source=ig_tumblr_share&igshid=12ipkqgejytsz
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webdizaynstudiya · 3 years
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8 Noyabr Zəfər Gününüz Mübarək! 🇦🇿Qarabağ Azərbaycandır! #Zəfər #ZaferGünü #8NoyabrZəfərGünü #Şuşa #Shusha #Susa #Qarabağ #Garabagh #Karabakh #FreeKarabakh #FreeShusha #8Noyabr #ZəfərGünü #ZeferGunu #ZaferGünü #Azerbaycan #Azərbaycan #Azerbaijan #ŞuşaQarabağ #QarabağAzərbaycandır #🇦🇿Qarabağ https://www.instagram.com/p/CWApx08t2U_/?utm_medium=tumblr
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futboldunyasi · 4 years
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🇦🇿🇦🇿🇦🇿Uğurlar "QARABAĞ"‼️🇦🇿🇦🇿🇦🇿 . . . #qarabağfk #qarabağ #garabaghfc #garabagh #karabakh #karabakhfc #villarreal #europaleague #europaleague2020 #footballworld #futboldünyası #futboldunyasi (at Başakşehir Fatih Terim Stadyumu) https://www.instagram.com/p/CG730ZhniMz/?igshid=mvzuuk0ng5om
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novellakitabevi · 4 years
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Əsgər payı💜 #novellakitabevi #qarabag #karabakhisazerbaijan #garabagh (at QARABAĞ) https://www.instagram.com/p/CFweu2xnLAS/?igshid=18r3a9rz36q61
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yoursaeidjavid · 5 years
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#garabagh #armenian #handmade #runnerscapriolese #swimtheisland #l #lesorghedelòi #lagodiiseo #girodellago #saeidjavid #duathlon #triathlon #fin #fidal #fitri #fci #sarnico #paratico #palazzolosulloglio #capriolo #runners #ciclet #corsamattutina (presso Campomatto, Sarnico) https://www.instagram.com/p/BwzM1XqA1uf/?utm_source=ig_tumblr_share&igshid=1k1mfgsiiz5p1
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bordoberelilerr · 3 years
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Dağlık Karabağ’da ateşkesi korumak için görev yapacak olan Türkiye-Rusya Ortak Merkezi; Azerbaycan Savunma Bakanı Org. Zakir Hasanov, Millî Savunma Bakan Yardımcısı Yunus Emre Karaosmanoğlu ve Rusya Savunma Bakan Yardımcısı Aleksandr Fomin’in katıldığı törenle açıldı. @savunmabakanligi (AGDAM. Garabagh. Azerbaycan) https://www.instagram.com/p/CKq877Bhdud/?igshid=n8vckay9oj89
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derekhaleismyheart · 4 years
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İ know i post very rarely, but his occasion is worth it. This past month has been a very hard month for my country, since september 27 2020 armenia has broke the ceasefire berween armenia and azerbaijan, provocating azerbaijanian army. Since then, a war has been going in both countries, resulting with armenias missile attacks at our cities far away from the war zone. They twice attacked the second biggest city of Azerbaijan, Ganja, at night. As a result, a lot of people got injured, and under 30 people died, while calmly sleeping in their houses. A big part of the dead are only kids. Yesterday they attacked Barda, which is NOT even close to the war zone, as a result nearly 4 civilians died and 14 got injured, 4 of the wounded being kids.
Explaining the reason of the war: 20% of Azerbaijani lands have been under Armenian occupation for almist 30 years. There have been more than 1,000,000 refugees from these territories almost for 30 years. These refugees were expelled from Karabakh due to Armenian vandalism. (Search #Khojaly Genocide) their motherlands(starting from 1988 till 1993) from their homes. #dontbelievearmenia
Armenia, with its fictitious history and fake “facts”, attracts world celebrities to its lies. to support armenians means to support #terrorism. Armenians burned our inchants in Khojaly(1992, Feb 25)
, raped our women and tortured our elderly people. Now time is up! We bare lies for 30 years, and now fed up. Azerbaijan is liberating its lands! The lands that belong to Azerbaijan by centuries! Changing their names wont help too, for example its NOT STEPANOKERBLT ITS KHANKENDI( from azerbaijanese khan is king, kend is village, so its king's village)
So tell me, are WE the guilty side for wanting our historical territories back?? My ancestors are from Shusha, Qarabagh. We grew up always hearing that armenia occupied most of our territories, grew up hoping that one day, we will get them back. So THAT DAY has come, and we trust our army. AZERBAIJAN ARMY ATTACKS ONLY THE SOLDIERS, WHEN THE ARMENIAN ARMY ATTACKS CIVILE PEOPLE AND KIDS. Armenians tell that people who live in Qarabagh arent toys to remove them from there so easily and return the territory, were WE toys when they attacked them at night, in winter, making them run into the forest and die of the cold? If you are interested in more details, please research for the Khojaly genocide. Why do armenians hate us so much? Because of their so called "Armenian genocide" caused by turks in 1915, for which they cant attack Turkey, a big and a very piwerful country, so they instead attack AZERI TURKS to get revenge. My heart breaks for the civile people dying, all of us are very scared that a bomb will fall right on our houses( even if I live in Baku, which is situated approximately in 400 km from the war zone)
PLEASE, REPOST IT AS MUCH AS YOU CAN, BE THE VOICE OF US, CIVILE PEOPLE, THE VOICE OF THE AZERI PEOPLE WANTING OUR GARABAGH BACK, BE THE VOICE OF GANJA, BARDA🙏( Gara means black in azerbaijanese, when bagh means garden) I wanted you to know the Azerbaijani side of the story, please reblog as much as you can. If interested, search in the internet " khojaly genocide" "pray for ganja" "pray for barda" The photos below are only a part of the reality, there are hundreds of injured and dead, the saddest of it is that a big part of the dead and injured are kids. AZERBAIJAN FIGHTS AND ATTACKS ONLY SOLDIERS, WHILE ARMENIA KILLS INNOCENT CHILDREN WHO HAD THEIR WHOLE LIFE TO LIVE! AS A TEEN, ME AND MY FRIENDS HAVE LIVED IN PANICK AND FEAR THIS PAST MONTH, BECAUSE NO ONE KNOWS WHEN WILL A MISSILE FALL ON OUR ROOFS.
#stoparmenianterrorism
#garabaghisazerbaijan
#prayforganja
#prayforbarda
PLEASE DONT STAY SILENT, REBLOG AND SHARE🙏🙏🙏
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metbuat · 2 years
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Head coach of "Olympiakos".
Head coach of “Olympiakos”.
“Olympiakos” head coach Michel Gonzalez attended the press conference held before the third round match of the UEFA Europa League group stage in Greece against “Garabagh”. Metbuat.org reports that the 59-year-old specialist said: We want to beat “Qarabag”. We don’t think about the result other than winning 3 points. We can do it. We know well which club we represent. My game philosophy is only…
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yalaninfo · 3 years
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"Qarabağ" FK H qrupunda liderliyə yüksəlib, play-off-a çıxışını təmin edib. #Qarabağ #Qarabag #Qarabagh #Garabag #Garabagh #Karabakh #QarabagFC #QarabağFK #KarabakhFC #UEFA #QurbanQurbanov #Europe #FreeKarabakh #YALANinfo #yalan @yalan.info www.YALAN.info (at Azerbaijan-Azerbaycan) https://www.instagram.com/p/CV3hNFZoOcn/?utm_medium=tumblr
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eldarmirzeliyev · 5 years
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Azərbaycan Respublikasının Prezidenti cənab İlham Əliyev : "Qarabağ Azərbaycandır və nida işarəsi”. #OurPresident #İlhamAliyev #Azerbaijan #MyPresident #Azərbaycan #Garabagh #Karabakh #Qarabağ https://www.instagram.com/p/B3LaaczFSRR/?igshid=1fmvntoc83fkz
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Iris Publishers
Study of the Agro-Industrial Properties of the Soil Cover of the Agjabadi Region in the Example of the Garadolag Administrative Village
Authored by ZH Aliyev
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It is known from the brief nature of the territory of the research district that the date of establishment of Agjabadi district - 08.08.1930 The territory - 1.76 thousand sq.m. km Population - 136.8 thousand people (January 1, 2020) Population density - 1 sq. km. km 78 people (January 1, 2020). Agjabedi district is located in Mil and Garabagh plains of Kur-Araz lowland. Agjabedi city and Sarvanlar, Kurds, Minakhorlu, Garavelli, Galabadin, Avshar, Muganli, Shahsevan, Koyuk, Tazakend, Khojavend, Salmanbeyli, Ashagi Avshar, Hindarkh, Imamgulu-beyli, Mirzahagverdili, Sarijali, Balakhrizli, Taynaq, Poinag , Sharafkhanli, Shotlanli, Shenlik, Husulu, Ranjbarlar, Boyat, Hajilar, Garakhanli, Hajibadalli, Pariogullar, Agabeyli, Garadolag, Mehrabli, Kabirli, Aran, Yeni Garadolag, Najaf-gulubeyli, Qiyameddinli, Shahsevan-Tazakand, Shahsevan-Tazakand, Includes Jafarbeyli and Yukhari Qiyameddinli villages. The relief of the region is flat, gradually rising from the north-east to the south-west. The surface of the area is composed of continental-alluvial and marine sediments of the Anthropogenic system. There is a clay deposit. The climate is temperate hot, dry subtropical. The average temperature is 1.2-1.7 ° C in January and 25-26 ° C in July. Annual precipitation is 300-500 mm. The river network is sparse. The Kura River flows along the north-eastern border, and the Gargar River flows through the central part. The Upper Karabakh canal passes through the region. There is a salt lake in the area. Gray-meadow, gray, meadow-gray soils are widespread. In the central part, saline and saline soils are found. The plants are of steppe and semi-desert type. There are bushes and sparse Tugay forests on the banks of the Kura River. Animals: gazelle, wolf, wild boar, jackal, fox, swamp beaver, badger, gray rabbit, Asia Minor sand mouse, etc. Birds: turkey, pigeon, black grouse, pheasant, etc. Aggol National Park is located in Agjabadi district. 15 species of animals, 20 species of fish and 40 species of plants have been recorded here. Agjabadi is mainly an agricultural region. Fruit growing, cotton growing, grain growing, silkworm breeding, animal husbandry, etc. developed.
Keywords: Soil formation; Soil cover; Gray-meadow; Light gray-meadow; Heavy clayey; Light clayey salinity; Salinity; Erosion
Introduction
The establishment of Garadolag village is connected with the name of Garadolag tribe. In the 18th century, Panahali khan moved some of the Garadolags to Karabakh as part of the Kangarli. .As a result of the Kura flood in 1938, the Garadolags were relocated from the Kurkiragi areas where they settled to the area where they now live. Here they created Garadolag and then Yeni Garadolag villages. Garadolag village has an area of 32.7 square kilometers and a population of 3139 people. The main occupations of the population are agriculture and animal husbandry.
The course of the study
In accordance with the requirements of the existing agroindustrial grouping, in April 2017, a soil survey was conducted in the administrative territory of Yeni Garadolag village of Agjabedi district and the following was determined:
The total area of the surveyed area is 2180.77 ha. Land survey works covered an area of 1802.75 hectares.
The area is divided into the following natural areas:
Planting 1760.78 ha
Dinc 15.53 ha
Clean pasture 26.00 ha
Perennial plantings 0.44 ha
Other lands 378.02 ha
During the study, 82 sections were excavated in the area and morphological features were described in genetic layers. Soil samples were taken from the excavated sections and the following analytical-laboratory researches were carried out on them and the results were analyzed:
• Hygroscopic moisture - by thermal method
• Granulometric composition - by Kaczynski’s pipette method
• General humus - by the method of Tyurin
• Total nitrogen - By calculation
• Carbonate - With a calcimeter device
• Absorbed Ca and Mg - by Ivanov method
• Absorbed Na - by Hedroyts method
• pH water suspension - with pH meter
Thus, based on the results of field soil research and laboratory analysis, a soil map was prepared on a topographic basis and a report was written. Archival materials were used in compiling the maps and writing the report. From the scale of Professor RH Mammadov in determining the granulometric composition was used.
Natural conditions
Geographical position: The studied area is bounded on the north-west and north by Avshar village, on the east by Garadolag village, on the south-east by Mehrabli village, on the south by Kabirli village, on the south-west by Aran village and on the west. Avshar and Aran villages of winter pasture No. 104 are bordered by territorial lands.
Relief: Relief, as a structure of the earth’s surface, is directly involved in the formation of land cover as a factor in soil formation. It plays an important role in changing chemical and biological processes, hydrothermal regime and microclimate. Thus, the distribution of solar energy and atmospheric sediments is directly related to relief. The relief of the studied area consists of sloping and wavy plains.
Climate: Climate is one of the important factors as a factor in soil formation. Agjabedi district is located in the Kur-Araz lowland, in the western part of the Mill plain. The climate of the area is temperate hot semi-desert and dry steppes with dry summers, weak humidification is characterized by hot summers. The average temperature in January is 1.8 0C, the average temperature in July is 260C. The average annual relative humidity is 73%. The annual rainfall is 332 mm, mainly in spring and autumn. 980 mm of possible evaporation from the surface cover per year. The average annual soil surface temperature is 180C (Table 1).
Vegetation: Vegetation is a key factor in the process of soil formation and the formation of soil cover. The increase in soil fertility with the formation of organic matter depends on the density of vegetation. Maintaining normal soil moisture, reducing the washing effect of water, preventing the formation and development of the erosion process are closely related to vegetation.
In the area we studied, we found sagebrush, wild clover, cattail, solid guramid, yellow flower, carnation, reed, yagtikan, invitation, meadow, etc. plants are widespread. Cultivated crops are also grown in the area.Soil-forming rocks. Soil-forming rocks affect the granulometric composition, chemical and mineralogical composition of the soil, causing the formation of soil profile and genetic layers. The chemical composition of the parent rock plays an important role in the process of soil formation. The richer the parent rock, the better the quality of the soil formed on it. Thus, the soils of the area under study were formed on alluvial sediments.
Ground cover. According to the results of field soil research and laboratory analysis, the following soil types and subtypes are widespread in the area.
• Gray-meadow soils
• Light gray-meadow soils
I. Gray-meadow soils
Gray-meadow soils cover 761.47 ha or 34.92% of the total area, spreading to the west and east of the study area.
These soils are due to their granulometric composition and soil layer thickness; 1) Divided into heavy clayey, thick, gray-meadow species.
To get acquainted with the characteristic morphological features of these soils, we give a description of section 29 excavated in the area.
• 0-23 cm gray, topavari, heavy clayey, solid, tubers and rhizomes, boiling, dry, the transition is clear
• 23-54 cm light gray, topavari, light clay, less solid, root residue, boils, slightly moist, the transition is gradual
• 54-89 cm light gray, small clump, light clay, less solid, insect tracts, boils, less moisture, the transition is gradual
• 89-127 cm grayish, small topavari, light clay, soft, rust spots, boils, less moisture, the transition is gradual
• 127-156 cm straw, not selected, light clay, soft, carbonate stains, boiling, wet It is clear from the morphological description of the section that the color of these soils is gray in the upper layer, light gray and gray in the middle layer, and straw in the lower layer. The structure is not selected on the top layer, topavari and small topavari on the middle layer, and on the bottom layer. The granulometric composition was heavy clayey, and the length of the profile was wool the rose is clay. The density is hard on the top layer and less hard and soft on the bottom layers.
Roots and rhizomes, root residues, insect tracts, rust and carbonate stains are found along the profile from new derivatives and marshes.
These soils are boiled under the influence of 10% hydrochloric acid (HCl).
Humidity is dry in the upper layer, slightly moist in the middle layers, and moist in the lower layer. Transitions to genetic layers are clear and gradual throughout the profile.
According to the results of laboratory analysis, the granulometric composition of gray-meadow soils is heavily clayey. Thus, the amount of physical clay in these soils is 47.80-49.18% in the upper layers, and the profile length is 47.80-55.84% (Table 2).
Table 2: I) Granulometric composition of gray-meadow soils (in absolute dry soil, in %).
The hygroscopic humidity of the main components varies between 4.1-5.3% throughout the profile.
Total humus is 2.07-2.23% in the upper layers, and the profile length is 1.09-2.23%. According to the total humus, the total nitrogen content is 0.10-0.17%. The amount of carbonate is 10.69- 13.68% throughout the profile. The pH in the water suspension is 8.20-8.33 units, which indicates that these soils are alkaline (Table 3).
The total amount of absorbed bases in gray-meadow soils is 28.40-32.95 mg. As a percentage, the Ca base is 62.08-63.74%, the Mg cation is 33.33-35.24%, and the Na cation is 2.68-3.17% (Table 4).
II. Light gray-meadow soils
Light gray-meadow soils cover 1041.28 ha or 47.75% of the total area, spreading to the north and south of the study area.
These soils are divided into the following types according to their granulometric composition and thickness of the soil layer.
• Light clay, thick, light gray-meadow
• Heavy clayey, thick, light gray-meadow
To get acquainted with the characteristic morphological features of these soils, we give a description of section 55 excavated in the area.
• 0-22 cm light gray, topavari, light clay, solid, rootand roots, boiling, dry, clear transition
• 22-55 cm light gray, topavari, light clayey, less solid, root residue, boil, dry u, the transition is gradual
• 55-88 cm grayish, small clumpy, lightly clayey, less solid, vertical cracks, boils, less moisture, gradual transition
• 88-122 cm grayish, small topavari, light clay, soft, rust stains, boils, less moisture, gradual transition
• 122-155 cm straw, not selected, light clay, soft, carbonate spots, boils, less moisture.
It is clear from the morphological description of the section that the color of these soils is light gray in the upper layer, light gray and gray in the middle layers, and straw in the lower layer. The structure is not selected on the top layer, topavari and small topavari on the middle layer, and on the bottom layer. The granulometric composition is light clay throughout the profile. The density is hard on the top layer and less hard and soft on the bottom layers. Roots and rhizomes, root residue, vertical cracks, rust and carbonate stains are found along the profile from new derivatives and alloys. These soils are boiled under the influence of 10% hydrochloric acid (HCl). Humidity is dry in the upper layers and less moist in the lower layers. Transitions to genetic layers are clear and gradual throughout the profile.
According to the results of laboratory analysis, the granulometric composition of light gray-meadow soils is light clayey and heavy clayey. Thus, the amount of physical clay in these soils is 45.16- 52.08% in the upper layers, and the profile length is 45.16-55.96% (Table 5).
The hygroscopic humidity of the main components varies between 4.3-5.3% throughout the profile. Total humus is 1.74- 1.96% in the upper layers, and the profile length is 0.76-1.96%. According to the total humus, the amount of total nitrogen is 0.08- 0.16%. The amount of carbonate is 10.26-14.11% throughout the profile. The pH in the water suspension is 8.19-8.34 units, which indicates that these soils are alkaline (Table 6).
The total amount of absorbed bases in light gray-meadow soils is 26.30-33.05 mg. The percentage of Ca cations is 60.41-63.41%, the Mg cation is 34.01-36.57%, and the Na cation is 2.44-3.28% (Table 7).
Acknowledgement
None.
Conflict of Interest
No conflict of interest
 To read more about this article: https://irispublishers.com/wjass/fulltext/study-of-the-agro-industrial-properties-of-the-soil-cover-of-the-agjabadi-region.ID.000625.php
  Indexing List of Iris Publishers: https://medium.com/@irispublishers/what-is-the-indexing-list-of-iris-publishers-4ace353e4eee
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