| تعداد نشریات | 286 |
| تعداد نشریات سازمان | 84 |
| تعداد شماره‌ها | 2,907 |
| تعداد مقالات | 32,799 |
| تعداد مشاهده مقاله | 43,064,239 |
| تعداد دریافت فایل اصل مقاله | 19,658,662 |
ارزیابی خشکسالی و مداخلات انسانی در کاهش ذخایر آب زیرزمینی | ||
| تحقیقات حمایت و حفاظت جنگلها و مراتع ایران | ||
| مقاله 13، دوره 20، شماره 1 - شماره پیاپی 39، مهر 1401، صفحه 199-218 اصل مقاله (1.68 M) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22092/ijfrpr.2022.356091.1513 | ||
| نویسندگان | ||
| سمیرا زندی فر* 1؛ عادل جلیلی2؛ زهرا سعیدی فر3؛ مریم نعیمی1 | ||
| 1استادیار پژوهش، بخش تحقیقات بیابان، مؤسسه تحقیقات جنگلها و مراتع کشور، سازمان تحقیقات، آموزش و ترویج کشاورزی، تهران، ایران | ||
| 2استاد پژوهش، بخش تحقیقات گیاه‌شناسی، مؤسسه تحقیقات جنگلها و مراتع کشور، سازمان تحقیقات، آموزش و ترویج کشاورزی، تهران، ایران | ||
| 3محقق، بخش تحقیقات بیابان، مؤسسه تحقیقات جنگلها و مراتع کشور، سازمان تحقیقات، آموزش و ترویج کشاورزی، تهران، ایران | ||
| چکیده | ||
| مدیریت و برنامه‌ریزی صحیح جهت جلوگیری از کاهش سطح آب زیرزمینی، نیازمند شناخت عوامل، شاخص‌ها و معیارهای تغییرات تراز آب زیرزمینی در مناطق تحت تأثیر این پدیده است. بنابراین برای آگاهی از وضعیت نوسانات سطح آب‌های زیرزمینی لازم است مطالعات دقیقی به منظور برنامه‌ریزی، بهره‌برداری و نگهداری طرح‌های توسعه منابع آب و پیش‌بینی و هشدار به موقع دوره‌های خشکسالی، صورت پذیرد. بدین منظور در مطالعه حاضر به بررسی روند تغییرات آب زیرزمینی در آبخوانهای محدوده مطالعاتی ماهیدشت در استان کرمانشاه در یک دوره آماری 35 ساله منتهی به سال 1396پرداخته شد. سپس تاثیر انواع خشکسالی ها بر روند تغییرات تراز آب زیرزمینی با استفاده از شاخص‌های خشکسالی PDSI، GRI و SDI و همچنین تغییرات سطح زیرکشت اراضی زراعی آبی و دیم مورد تجزیه و تحلیل قرار گرفت. بر اساس نتایج بالاترین سطح آب زیرزمینی مربوط به نواحی جنوب شرقی و حدود 1531 متر است. تغییرات سطح آب زیرزمینی در دشت ماهیدشت به طور کلی روندی نزولی دارد و سطح آب زیرزمینی در طول دوره مطالعاتی با افتی برابر 78/24 متر روبرو بوده است. همچنین نتایج همبستگی پایین دو شاخص خشکسالی اقلیمی و آب های سطحی با آب‌های زیرزمینی نشان دادکه عامل افت سطح آب در آبخوانهای دشت بر اثر عدم مدیریت و برداشت‌های بی‌رویه می باشد. اگرچه آبخوان ماهیدشت به عنوان مطالعه موردی در این مقاله انتخاب شده است، روش پیشنهادی می تواند در مناطق دیگر نیز برای بهبود حفاظت و مدیریت منابع آب استفاده شود. | ||
| کلیدواژه‌ها | ||
| نوسانات سطح آب زیرزمینی؛ حفاظت و مدیریت منابع آب؛ آبخوان ماهیدشت؛ خشکسالی | ||
| عنوان مقاله [English] | ||
| Assessing drought and human Interface on reducing groundwater reserves | ||
| نویسندگان [English] | ||
| Samira Zandifar1؛ A. Jalili2؛ zahra saieedifar3؛ Maryam Naeimi1 | ||
| 1Desert Research Division, Research Institute of Forests and Rangeland, Agricultural Research, Education and Extension Organization (AREEO), Tehran, Iran | ||
| 2Botany Research Division, Research Institute of Forests and Rangeland, Agricultural Research, Education and Extension Organization (AREEO), Tehran, Iran | ||
| 3Desert Research Division, Research Institute of Forests and Rangeland, Agricultural Research, Education and Extension Organization (AREEO), Tehran, Iran | ||
| چکیده [English] | ||
| Proper management and planning to prevent the decline of groundwater levels, requires knowledge of the factors, indicators and criteria for changes in groundwater levels in areas affected by this phenomenon. Therefore, in order to be aware of the status of groundwater level fluctuations, it is necessary to conduct detailed studies in order to plan, operate and maintain water resources development plans and to predict and warn in time of drought periods. For this purpose, in the present study, the trend of groundwater changes in aquifers of Mahidasht study area in Kermanshah province in a statistical period of 35 years ending in 1396 was investigated. Then, the impact of droughts on the trend of groundwater level changes was analyzed using PDSI, GRI and SDI drought indices as well as changes in irrigated and rainfed arable lands. According to the results, the highest groundwater level is in the southeast and is about 1531m. Groundwater level changes in Mahidasht plain are generally declining and the groundwater level has dropped by 24.78m during the study period. Also, the results of low correlation between climatic and groundwater drought indices showed that the cause of water level decline in plain aquifers due to irregular impressions and management. Although Mahidasht aquifer has been selected as a case study in this article, the proposed method can be used in other areas to improve the protection and management of water resources. | ||
| کلیدواژه‌ها [English] | ||
| Groundwater level fluctuations, protection and management of water resources, Mahidasht aquifer, drought | ||
| مراجع | ||
|
-Allen, R.G., Pereira, L.S., Rase, D. and Smith, M., 1998. Crop Evapotranspiration: Guidelines for Computing Crop Requirements, Irrigation and Drainage Paper No. 56, FAO Rom, Italy, 300p. -Azadi, S., Soltani Kopaei, S., Faramarzi, M., Soltani Tudeshki, A. and Pourmanafi, S., 2015. Evaluation of palmer drought severity index in central Iran. JWSS, 19(72): 305-319. -Bazrafshan, J. and Khalili, A., 2013. Spatial analysis of meteorological drought in Iran from 1965 to 2003. Desert, 18(1): 63-71. -Fishman, R.E., 2011. Using water balance models to approximate the effects of climate change on spring catchment discharge: Mt. Hanang, Tanzania. (MS Thesis, Michigan Technological University). Available at: http://www.geo.mtu.edu/rs4hazards/Project%20resources/theses/fish_thesis.pdf. -Fisher, P.F.; 2005. Development in spatial data handling, Springer, Germany, 676p. -Fiorillo, F., Esposito, L. and Guadagno, FM., 2010. Karst spring discharges analysis in relation to drought periods, Using the SPI. Water Resources Manage, 24: 1867-1884. -Gehreles, J.C., Van Geer, F.C. and De Vries, J.J., 1994. Decomposition of groundwater level fluctuations using transfer modeling in an area with shallow to deep unsaturated zones. Journal of Hydrolog., 157: 105-138. -Halder, S., Roy, M.B. and Roy, P.K., 2020. Analysis of groundwater level trend and groundwater drought using Standard Groundwater Level Index: a case study of an eastern river basin of West Bengal, India. SN Applied Sciences, 2(507): 507-531. -Havril, T., Tóth, Á., Molson, J.W., Galsa, A. and Mádl-Szőnyi, J., 2018. Impacts of predicted climate change on groundwater flow systems: Can wetlands disappear due to recharge reduction? Journal of Hydrology, 563: 1169-1180. -Hellwing, J., de Graaf, I.E.M., Weiler, M. and Stahl, K., 2020. Large scale assessment of delayed groundwater responses to drought. Water Resource, 56(2): 1-19. -Khosravi Dehkordi, A., Mirabbasi, R., Samadi Boroujeni, H. and Ghasemi Dastgerdi, A.R., 2019. Monitoring and forecasting of groundwater drought in Shahrekord plain using Groundwater Resource Index (GRI) and Markov chain model. Hydrogeology, 4(1): 111-125 (In Persian) -Konikow, L.F. and Kendy, E., 2005. Groundwater depletion: A global problem. Hydrogeology Journal 13(1): 317-320. -Liu, L., Hong, Y., Bednarczyk, C.N., Yong, B., Shafer, M.A. and Riley, R., 2012. Hydro climatological drought analyses and projections using meteorological and hydrological drought indices: a case study in Blue River Basin Oklahoma. Water Resources Management, 26(10): 2761-2779. -McKee, T.B., Doesken, N.J. and Kleist, J., 1993. The relationship of drought frequency and duration to time scales. Eight Conference on Applied Climatology, Anaheim, CA, American Meteorological Society, pp. 179-184. -Mair, A. and Fares, A., 2010. Influence of groundwater pumping and rainfall spatio-temporal variation of stream flow. Journal of Hydrology, 393: 287-308. -Mendicino, G., Senatore, A. and Versace, P., 2008. A Groundwater Resource Index (GRI) for drought monitoring and forecasting in a Mediterranean climate. Hydrology Journal, 357: 282-302. -MesbahZadeh, T. and SoleimaniSardoo, F., 2018. Temporal trend study of hydrological and meteorological drought in Karkheh watershed. Jwmseir, 12 (40):105-114 (In Persian). -Mofidipoor, N., Brady Sheikh, V. and Ownegh, M., 2011. Sydaldyn A. the analysis of relationship between meteorological and hydrological droughts in Atrak. Watershed jwmr, 3(5): 16-26 (In Persian). -Mirakbari, M., Mortezaii, G. and Mohseni, M., 2018. Investigation of Effect Meteorological Drought on Surface and Ground Water Resources by Indices SPI, SPEI, SDI and GRI. Journal of Watershed Management Science and Engineering, 12(42):70-80 (In Persian). -Mohammadi, S., Salajegheh, A., Mahdavi, M. and Bagheri, R., 2012. An ivestigation on spatial and temporal variations of groundwater level in Kerman plain using suitable geostatistical method (During a 10-year period). Iranian Journal of Range and Desert Reseach, 19(1): 61-70 (In Persian). -Moustadraf, J., Razack, M. and Sinan, M., 2003. Evaluation of the impacts of climate changes on the coastal Chaouia aquifer, Morocco, using numerical modeling. Hydrogeology Journal, 16(7): 1411-1426. -Moravej, M., Khalili, K. and Behmanesh, J., 2015. Investigation of relationship between hydrologic processes of precipitation, evaporation and stream flow using linear time series models (Case study: Western Basins of lake Urmia). Water and Soil, 29(1): 85-101 (In Persian). -Nalbantis, I., 2008. Evaluation of a hydrological drought index. Water Europe, 23: 67-77. -Nayak, P., Satyaji, R. and Sudheer, K.P., 2006. Groundwater level forecasting in a shallow aquifer using artificial neural network approach. Water Resources Management, 2: 1. 77-99. -Palmer, W.C., 1965. Meteorological Drought. Research. Paper No. 45, U. S. Department of Commerce Weather Bureau, Washington, D.C, 58p. -Peters, E., 2003. Propagation of drought through groundwater systems, Illustrated in the Pang (UK) and Upper-Guadiana (ES) catchments, Dissertation Wageningen Universiteit, Wageningen, 202p. -Russo, T.A. and Lall, U., 2017. Depletion and response of deep groundwater to climate-induced pumping variability. Nature Geoscience, 10(2): 105-108. -SoleimaniSardoo, F. and Bahremand, A., 2014. Hydrological drought analysis using SDI index in Halilrud basin of Iran. Journal of Environmental resources Research, 2(1): 47-56. -Sophocleous, M., 2000. From safe yield to sustainable development of water resources- the Kansas experience. Journal of Hydrology, 235: 27-43. -Thornthwaite, C.W., 1948. An approach toward a rational classification of climate. Geographical Review, 38: 55-94. -Van Loon, A.F., 2013. On the propagation of drought. Wageningen University, publication place, 196p. -Vicente-Serrano, S.M., Beguer’ia, S. and López-Moreno, J.I., 2010. A multiscalar drought index sensitive to global warming: the standardized precipitation evapotranspiration index. Journal of Climate, 23(7): 1696-1718. -Wang, M., Jiang, SH., Ren, L., YuXu, CH., Menzel, L., Yuan, F., Xu, Q., Liu, Y. and Yang, X., 2021. Separating the effects of climate change and human activities on drought propagation via a natural and human-impacted catchment comparison method. Journal of Hydrology, 603: 126913. -Williams, A.P., Seager, R., Abatzoglou, J.T., Cook, B.I., Smerdon, J.E., Cook, E.R., 2015. Contribution of anthropogenic warming to California drought during 2012–2014. Geophysical Research Letters, 42(16): 6819-6828. -Zandifar, S., Fijani, E., Naeimi, M. and Khosroshahi, M., 2020. Spatiotemporal variations of groundwater drought indices, Case study: Zohreh- Jarrahi watershed. Hydrogeology, 4(2): 108-130 (In Persian). -Zandifar, S., Dargahian, F., Fijani, E. and Naeimi, M., 2021. The trend of groundwater variations and drought in the Karkheh watershed. Watershed Management Research Journal, 34(3): 53-73 (In Persian). -Zareii, H., Kalantari, N. and Nadri, A., 2017. Climate changes effects on quantity and quality conditions of the Bibitalkhone Karstic Spring, Lali Khuzestan. Hydrogeology, 2(2): 1-16 (In Persian). -Zhang, L., Jiaoa, W., Zhanga, H., Huanga, C. and Tonga, Q., 2017. Studying drought phenomena in the Continental United States in 2011 and 2012 using various drought indices. Remote Sensing of Environment, 190: 96-106. -Zynali, B., Asghari Saraskanroud, S. and Saffarian Zangir, V., 2017. Monitoring and forecast of drought in Urmia lake basin by SEPI index and ANFIS Model. Journal Spatial Analysis of Environmental Hazards, 4(1): 73-96 (In Persian). | ||
|
آمار تعداد مشاهده مقاله: 701 تعداد دریافت فایل اصل مقاله: 334 |
||