You searched for: seemingly simple function (Engelska - Persiska)

so i want to suggest that pleasure is deep -- and that this isn't true just for higher level pleasures like art, but even the most seemingly simple pleasures are affected by our beliefs about hidden essences.
بنابراین می خوام بگم که لذت منشا عمیقی داره-- این فقط درباره لذت های سطح بالا مثل هنر نیست، بلکه درباره لذت های به ظاهر خیلی ساده ای که اعتقادمون بر روی ماهیت پنهانشان تاثیر گذاشته هم مصداق داره.

in einstein's theory, it turns out to be impossible to find a general definition for a seemingly simple property such as a system's total mass (or energy).
در نظریه اینشتین مشخص می‌گردد که غیر ممکن است که بتوان یک تعریف عمومی برای ویژگی ظاهراً ساده‌ای مانند جرم (انرژی) کل یک سیستم ارائه داد.

for an example, consider a simple function definition in haskell syntax (function parameters are not in parentheses but are separated by spaces, = is not assignment but definition):here, 0 is a single value pattern.
به عنوان مثال، يک تابع haskell با سينتکس ساده را فرض کنيد( پارامتر های تابع در پرانتز نمی آيند، = به معنای مساوی نيست، بلکه به معنی تعريف است):در اينجا، 0 يک الگو ی تک مقداری است.

both the evolution of the erosion rate with depth and the maximum depth of erosion can be defined as simple functions of the general characteristics of the flow and the fine and coarse fractions of the sediment. the proposed approach will lead to improved estimates of the conditions under which fine sediments that have infilled gravel beds are re entrained.
هم تکامل نرخ فرسایش با عمق و هم حداکثر عمق فرسایش را می توان به عنوان توابع ساده از ویژگی های کلی جریان و بخش های ریز و درشت رسوب تعریف کرد. رویکرد پیشنهادی منجر به برآوردهای بهبود یافته از شرایطی می‌شود که در آن رسوبات ریز که بسترهای شن پر شده دارند دوباره حباب می‌شوند.

an experimental nonintrusive methodology is proposed to estimate the spatially averaged erosion rate of fine sediment from a gravel bed. the experiments performed in a laboratory flume show a progressive slowdown of the erosion rate as the level of fine sediment becomes deeper within the gravel matrix, until a maximum depth of erosion is reached. two original relations are proposed for the maximum cleanout depth and the erosion rate based on a dimensional analysis applied to the experimental results. the proposed erosion rate relation modifies the original van rijn formula for a uniform bed, introducing a damping function below the gravel crest. both the evolution of the erosion rate with depth and the maximum depth of erosion can be defined as simple functions of the general characteristics of the flow and the fine and coarse fractions of the sediment. the proposed approach will lead to improved estimates of the conditions under which fine sediments that have infilled gravel beds are re-entrained. this will help inform strategies aimed at restoring degraded river systems and mitigating the undesired side effects of activities such as sediment flushing which can result in colmation.
چارچوب مفهومی جدید برای فرسایش رسوبات ریز از یک ماتریس شن بر اساس تجزیه و تحلیل تجربی