رام بابو سکسینہ
افسوس ہے دسمبر کے آخری ہفتہ میں جناب رام بابو سکسینہ کاحرکت قلب بند ہوجانے سے بحالت سفر اچانک انتقال ہوگیا۔ موصوف کو اردو زبان وادب کے ساتھ عشق تھااوروہ اس کا بڑا وسیع اورگہرا مطالعہ رکھتے تھے۔یہی وجہ ہے کہ ایک ذمہ دار سرکاری عہدہ کی چند درچند مصروفیتوں کے باوجود انھوں نے ادبِ اردو پرمتعدد ضخیم کتابیں اپنی یادگار چھوڑی ہیں۔ ان کی کتاب ’تاریخ ادبِ اردو‘ کو بڑی مقبولیت حاصل ہوئی، اس موضوع پر یہ کتاب اس پایہ کی ہے کہ ادبِ اردو کاکوئی طالب علم اس سے بے نیاز نہیں ہوسکتا۔اس کے علاوہ’’اردو کے انگریز شعرا‘‘ نامی کتاب انھوں نے بڑی تلاش وجستجواورمحنت سے مرتب کی تھی۔ایک کتاب حال میں ہی’’مرقع شعراء‘‘کے نام سے شائع ہوئی ہے۔سنا ہے کہ دو کتابوں کے مسودے ابھی اورباقی ہیں جو غیر مطبوعہ ہیں،موصوف اب دنیا میں نہیں لیکن اُن کے یہ شاندار ادبی کارنامے اُن کانام زندہ رکھیں گے۔
[جنوری۱۹۵۸ء]
The Figures of Speech(ملع عيدبلا )is a Significant branch of Arabic Rhetoric. It has two kinds; Literal Aesthetic, تانسحملا ةيظفللا)) Semantic Aesthetic, (تانسحملا ةيظفللا). Both kinds are having a pivotal role in the miracle of Qurān. The Great Scholar of Rhetoric Al-Zamakhshari has mentioned many of its types to analyze the Qurānic Verses rhetorically in his exegesis Al-Kashāf. The Great Scholar Abd Al-Qāhir Al-Jurjāni did not approach the upper mentioned kinds, not for the reason of non-interference in The Qurānic miracles but he was always eager to derive new ideas in this particular field. As it is known that many former scholars have approached all kinds of the Figures of Speech in a wide range and Abd Al-Q┐hir Al-Jurjāni was dominated by his creative nature. In this article, it has been discussed widely the academic ambivalence surrounding Abd Al-Q┐hir Al-Jurjāni's lack of interest in the Figures of Speech among three modern scholars: Dr. Muhammad Ahmad Al-ķwfi, Dr. Muhammad Shwq┘ Zaif, Dr. Muhammad Ab┴ Mosā.
Temporal variability of flows and sediments and bank erosion is fundamental to understand river dynamics. The temporal variability of sediment load and effective discharge class is one of essential information which is require to improve the barrage and canal operations for flow diversion into the canals. Similarly, bank erosion causes substantial land loss along the river banks due to erosion. Moreover, understanding for the impact of flood events on bank erosion are also lacking for sand bed braided river reaches. Similarly, quantitative relationship between branch channel movement and river bank erosion also have not attained significant attention. The river reach just starting from downstream of the Marala barrage to the 7 km downstream was selected to study the bank erosion. The reach is braided with small unstable sand bars and few semi-stable islands and river flows in multiple channels during low flows. The major proportion of the flows in the Chenab River occurs during monsoon season, which brings lot of sediments from the catchment. Thus, sediments in the river flows not only cause changes in the morphology of river but also diversion of highly sediment laden flows into the canals which creates sedimentation issues. Therefore, firstly, sediment rating curve, variation of sediment load and effective discharge for different temporal scales were examined. Secondly, the changes in the river were assessed and the relationships of river bank erosion with branch channels movement and floods magnitudes (during different flow regimes) were developed. Thirdly, two dimensional (2D) hydrodynamic numerical model was simulated for the flows/floods of 2010 and the results were coupled with the excess shear stress approach to predict the bank erosion and identify the river bank locations more vulnerable to erosion.