دانلود رایگان مقاله اثر سرریز و نفوذ اتصال در بی ثباتی سونامی ناشی از موج شکن کیسون

عنوان فارسی
اثر سرریز و نفوذ اتصال در بی ثباتی سونامی ناشی از موج شکن کیسون
عنوان انگلیسی
Effect of overflow and seepage coupling on tsunami-induced instability of caisson breakwaters
صفحات مقاله فارسی
0
صفحات مقاله انگلیسی
9
سال انتشار
2016
نشریه
الزویر - Elsevier
فرمت مقاله انگلیسی
PDF
کد محصول
E2943
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مهندسی عمران
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سازه های دریایی
مجله
مهندسی ساحلی - Coastal Engineering
دانشگاه
موسسه بندر و فرودگاه تحقیقات، موسسه ملی صنایع دریایی، بندر و فناوری حمل و نقل هوایی، ژاپن
کلمات کلیدی
سونامی، سرریز، صیقلی کردن، نفوذ، موج شکن کیسونی، تپه قلوه سنگ
۰.۰ (بدون امتیاز)
امتیاز دهید
چکیده

Abstract


In this study, a new tsunami overflow-seepage-coupled centrifuge experimental system was developed and applied to investigate the concurrent processes, and to elucidate the mechanism, of the instability involving the scour of the mound/sandy seabed, bearing capacity failure and flow of the foundation, and the failure of caisson breakwaters, with high-resolution image analysis. A series of experiments were conducted with and without the effects of the seepage by keeping the same overflow conditions (water volume, overflow velocity, fall height and water depth), and with different mound cross-sections. All of the experiments were conducted under 50 gravities and comprised of 3 series. The first series of experiments targeted the instability of the mounds themselves by constraining the caisson movement (sliding and overturning). The second series of experiments then allowed the caisson movement and clarified how the mound scour would affect the overall stability of the caissons. The third series of experiments examined the effect of a countermeasure on the basis of the results from the two series of experiments. The experimental results first demonstrated that the coupled overflow-seepage actions promoted the development of the mound scour significantly. Notably, the scour front developed in the form of progressive slip failure at the vicinity of caissons, regardless of the mound thickness. This stems from the fact that the development of the mound scour shortened the seepage path around the shoulder area of the mound, enhancing the coupling effect of the overflow and seepage. Indeed, the scour stopped far from the caisson toe in the absence of seepage without affecting the stability of the caissons. By contrast, the scour development due to the coupled overflow-seepage approached the caisson toe and brought about bearing capacity failure of the mound, resulting in the total failure of the caisson breakwater, which otherwise remained stable without the coupling effect. The velocity vectors obtained from the high-resolution image analysis illustrated the series of such concurrent scour/bearing-capacity-failure/flow processes leading to the instability of the breakwater. The influence of placing an embankment as a countermeasure was also examined by employing different bank thickness. It is shown that the stability of the breakwaters was significantly improved with decreasing hydraulic gradient that manifested underneath the caissons due to the embankment effect. These findings will facilitate better assessment and improvement of the stability of caisson breakwaters with rubble mound foundations.

نتیجه گیری

4. Conclusions


In the present study, a new centrifuge experimental system that is capable of controlling the coupling actions of overflow and seepage due to a tsunami was developed to investigate tsunami-induced instability of caisson breakwaters with rubble mound foundations. The system was used with high-resolution digital image correlation analysis by means of a high-speed CMOS camera. The principal findings and conclusions obtained from three series of experiments are summarized below.The results from the first and part of the second series of experiments demonstrated the way in which the scour front developed accompanying progressive slip failure of the rubble mounds, irrespective of the mound thickness. By contrast, the scour stopped far from the caisson toe in the absence of the seepage. It was found that the coupled overflow and seepage promoted the development of the mound scour considerably in the vicinity of caissons. This stemmed from the fact that the scour development shortened the seepage path, that promoted the seepage, enhancing the coupling effect of the over- flow and seepage. These results gave rise to a distinct scour mechanism in the form of the progressive slip failure of the mound. The occurrence of washout and boiling as a consequence of the coupled overflow and seepage were also demonstrated, yielding a cavity formation beneath the caissons.


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