نتایج جستجو برای: variography

تعداد نتایج: 64  

2001
Brian A. Needelman William J. Gburek Andrew N. Sharpley Gary W. Petersen

management (Lemunyon and Gilbert, 1993). The P index accounts for source (soil P and rate, method, and The mapping of soil P concentration is necessary to assess the timing of applied P) and transport (surface runoff, erorisk of P loss in runoff. We modeled the distribution of Mehlich-3 sion, leaching, and landscape position) factors controlextractable soil P (M3P) in an east-central Pennsylvan...

Journal: :فیزیک زمین و فضا 0
شیما سلیمانی دانشجوی کارشناسی ارشد ژئوفیزیک، گروه فیزیک زمین، موسسه ژئوفیزیک دانشگاه تهران، ایران امید اصغری استادیار، دانشکده معدن، دانشگاه تهران، ایران محمدکاظم حفیظی استاد، گروه فیزیک زمین، موسسه ژئوفیزیک دانشگاه تهران، ایران

saltwater intrusion into freshwater in coastal areas has been a serious concern for many countries. providing fresh water in some regions is very crucial. in fact, the areas that  are prone to encountering salt water zones should be checked meticulously. the preferred method for such investigation is a precise 3-d model of distribution of fresh and salt water in order to reach such a model, rel...

Journal: :فیزیک زمین و فضا 0
کیوان نجف زاده دانشجوی کارشناسی ارشد، گروه فیزیک زمین، موسسه ژئوفیزیک، دانشگاه تهران، ایران محمدعلی ریاحی دانشیار، گروه فیزیک زمین، موسسه ژئوفیزیک دانشگاه تهران، ایران محسن سیدعلی کارشناس ارشد مهندسی اکتشاف نفت، تهران، ایران

permeability is a key parameter in reservoir characterization. in fact, without accurate information about reservoir permeability, there is no good solution for reservoir engineering problems. up to now, permeability values of a reservoir have been calculated through laboratory measurements or well testing methods. these methods are useful but they cannot describe a reservoir reliably and preci...

2010
Alejandro Cáceres

Truncated Gaussian simulation (TGS) and plurigaussian simulation (PGS) are widely accepted methods for generating realisations of geological domains (lithofacies) that reproduce contact relationships. The realisations can be used to evaluate transfer functions related to the lithofacies occurrence, the simplest ones of which are the probability of occurrence of each lithofacies and the most pro...

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