|
|
بررسی تناسب اقلیمی نخود (cicer arietinum l.)، براساس شاخصهای دوره رشد و بارش در استان کردستان
|
|
|
|
|
نویسنده
|
چراغی حمید ,قنبری احمد ,اصغری پور محمدرضا ,طائی سمیرمی جواد ,حسامی علی
|
منبع
|
بوم شناسي كشاورزي - 1402 - دوره : 15 - شماره : 3 - صفحه:625 -642
|
چکیده
|
توزیع، شدت، مدت و نوع نزولات آسمانی در مراحل مختلف کشت، سبز شدن، پنجه زنی، تشکیل ساقه و گلدهی نخود (cicer arietinum l.)، اهمیت بسزایی دارد. از طرفی، ریسک یا عدم قطعیت یک عامل بسیار مهم در ارزیابی خطرات آب و هوایی و اثربخشی استراتژیهای مختلف در سیاستهای کشاورزی است. هر ریسک اقلیمی توسط خصوصیات طبیعی خود، شامل خصوصیات جغرافیایی، زمان وقوع و شدت ریسک شناخته میشود. این مطالعه بهمنظور برآورد ریسک بالقوه تولید نخود دیم در استان کردستان انجام شد. دادههای درازمدت اقلیمی از 15 ایستگاه برای دوره زمانی بیست ساله 1370 تا 1390 جمعآوری گردید. نتایج نشان داد که استان کردستان به سه منطقه اقلیم زراعی تقسیم گردید؛ منطقه پر ریسک یا نامناسب اقلیم- زراعی (0.23 درصد از کل منطقه)، منطقه با ریسک متوسط یا با تناسب نسبی برای تولید (59.71 درصد از کل منطقه)، منطقه کم ریسک یا مناسب اقلیم- زراعی (37.96 از کل منطقه). نتایج حاصل از بررسی ارتباط بین بارندگی مرحله رویشی و پتانسیل کشت نخود دیم منطقه نشان داد، بهجز قسمتهای ناچیزی از شهرستان های قروه و بیجار و سروآباد که در درجه ضعیف میباشند. کل منطقه از لحاظ تامین رطوبت مورد نیاز در درجه بسیار مطلوبی قرار دارد که دلیل این امر نیز بروز بارندگی لازم در این دوره زمانی و رطوبت ذخیره شده از نزولات زمستانه می باشد. وقوع نزولات مناسب برای دوره رشد رویشی در کل منطقه دارای بیشترین مقدار نسبت به دیگر مراحل نموی بوده است.
|
کلیدواژه
|
پارامترهای بارندگی، دوره رشد، روز بیولوژیک، سیستم اطلاعات جغرافیایی
|
آدرس
|
دانشگاه زابل, دانشکده کشاورزی, گروه زارعت, ایران, دانشگاه زابل, دانشکده کشاورزی, گروه زراعت, ایران, دانشگاه زابل, دانشکده کشاورزی, گروه زراعت, ایران, دانشگاه فنی حرفهای تهران, گروه علوم کشاورزی, ایران, مرکز تحقیقات و آموزش کشاورزی و منابع طبیعی استان کردستان, ایران
|
پست الکترونیکی
|
ali.hesami@areo.ir
|
|
|
|
|
|
|
|
|
agroclimatic suitability assessment for rain- fed chickpea (cicer arietinum l.) based on growth period and precipitation indices in kurdistan province
|
|
|
Authors
|
cheraghi hamid ,ghanbari ahmad ,asgharipour mohammad reza ,taei samirmi javad ,hesami ali
|
Abstract
|
introduction rainfall is a predominant climatic element that affects the density and location of agricultural systems as well as the choice of farming operations. the distribution, intensity, duration, and type of rainfall are very important at different stages such as cultivation, emergence, tillering, stem formation, and flowering. kurdistan province has regular rainfall with an average rainfall of more than 500 mm per year. therefore, kurdistan province is one of the most prone rain-fed areas in iran. as well his province with an area under cultivation of 120,000 hectares is one of the most important areas of chickpea growing in the country. however, the distribution of rainfall is not the same in all regions of this province, and therefore it is necessary to study the potential risk of chickpea production in kurdistan province. materials and methodslong-term climatic data were collected from 15 stations for a period of 20 years from 1991 to 2011. the results of spatial and temporal analysis determined the climatic-agronomic indices of the suitable region and the amount of dryland chickpea production. kurdistan province was divided into three climatic regions; high-risk or unsuitable climatic-agro-area (0.23% of the total area), medium-risk area or with relative proportion for production (59.71% of the total area), low-risk or suitable climatic-agro-area (37.96%) from the whole area). results and discussionthe results of spatial and temporal analysis determined the climatic-agronomic indices of the suitable region and the amount of dryland chickpea production. kurdistan province was divided into three climatic regions; high-risk or unsuitable climatic-agro-area (0.23% of the total area), medium-risk area or with relative proportion for production (59.71% of the total area), low-risk or suitable climate-agro-area (37.96%) from the whole area). the results of the study on the relationship between rainfall of vegetative stage and the potential of cultivation of dryland chickpeas in the region show except for a small part of qorveh, bijar, and sarvabad cities which are in a weak degree. the whole region is in a very good degree in terms of supplying the required moisture, which is also due to the necessary rainfall at this time and the humidity of the storage capacity stored from the winter rains. the occurrence of suitable precipitations for the vegetative period in the whole region had the highest value compared to other developmental stages. the results of the study between the relationship between reproductive stage rainfall and cultivation potential of rainfed chickpeas in the region showed that zarrineh station in the north of the region is weak due to unfavorable weather conditions at the beginning of the growing season and the developmental stages of the growing season in this region are delayed. at zarrineh station, the critical reproductive stage occurs at a time of year when the probability of precipitation in kurdistan has actually decreased and a part of the southeast of qorveh city is one of the weak and critical areas. the rest of the province in terms of moisture supply for this stage of dryland chickpea development is in a suitable degree, which is due to the necessary rainfall in this period of development. conclusionthe results of the study show the relationship between rainfall of vegetative stage and cultivation potential of dryland chickpeas in the region, except for a small part of qorveh, bijar and sarvabad counties, which are in a weak degree. the whole region is in a very good degree in terms of supplying the required moisture, which is also due to the necessary rainfall at this time and the humidity of the storage capacity stored from the winter rains. occurrence of suitable precipitations for the vegetative period in the whole region had the highest value compared to other developmental stages.
|
Keywords
|
biological day ,gis ,growth period ,rainfall parameters
|
|
|
|
|
|
|
|
|
|
|