東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Laboratory investigation of bedform ...

Messaros, Roy C.

FindBook

Google Book

Amazon

博客來

Laboratory investigation of bedform geometry under regular and irregular surface gravity waves.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Laboratory investigation of bedform geometry under regular and irregular surface gravity waves./
作者:	Messaros, Roy C.
面頁冊數:	229 p.
附註:	Source: Dissertation Abstracts International, Volume: 65-03, Section: B, page: 1497.
Contained By:	Dissertation Abstracts International65-03B.
標題:	Engineering, Marine and Ocean. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3127365

Laboratory investigation of bedform geometry under regular and irregular surface gravity waves.
Messaros, Roy C.

Laboratory investigation of bedform geometry under regular and irregular surface gravity waves. - 229 p.

Source: Dissertation Abstracts International, Volume: 65-03, Section: B, page: 1497.

Thesis (Ph.D.)--Stevens Institute of Technology, 2004.

Bedform geometry is an important feature in the near-shore bottom profile that can effectively enhance wave energy dissipation. Bedform geometry will regulate wave transformations and influence the sediment transport phenomenon. We begin with a historical review of the available literature. Next, a laboratory investigation of bedform geometry under regular and irregular surface gravity waves was conducted for two different depths in Towing Tank III at Davidson Laboratory. This wave tank facility provided an ideal opportunity for investigating bedform features for a flat bed and enabled the novel study of a sloped sediment bed. Our results provide new data that strengthens prior relationships and demonstrate that a sloped surface may be modeled in similar fashion to a flat sediment bed. These results also suggest that ripple dimensions may be independent of water depth and bottom orbital excursion amplitude (Ab) which is in contrast to the continental shelf under equilibrium conditions where ripples scale with Ab. The evaluation of wave tank dynamics was also conducted using an Acoustic Doppler Velocimeter (ADV) and surface wave data. Velocity measurements were performed using the ADV, and the wave records were measured using wave wire devices. The resulting data provided the basis for evaluating the hydrodynamics within the wave tank. Data analysis includes measurements of residual velocity and return flows that are inherent in a laboratory facility in the presence of propagating waves. The higher order harmonics that occur in laboratory facilities in the presence of monochromatic waves were evaluated as well. This information provides a new assessment of the hydrodynamics within Davidson Laboratory.Subjects--Topical Terms:

1019064
Engineering, Marine and Ocean.

Laboratory investigation of bedform geometry under regular and irregular surface gravity waves.
LDR:02617nmm 2200265 4500 001 1861527
005 20041117064930.5
008 130614s2004 eng d
035 $a (UnM)AAI3127365
035 $a AAI3127365
040 $a UnM $c UnM
100 1 $a Messaros, Roy C. $3 1949122
245 1 0 $a Laboratory investigation of bedform geometry under regular and irregular surface gravity waves.
300 $a 229 p.
500 $a Source: Dissertation Abstracts International, Volume: 65-03, Section: B, page: 1497.
500 $a Adviser: Michael S. Bruno.
502 $a Thesis (Ph.D.)--Stevens Institute of Technology, 2004.
520 $a Bedform geometry is an important feature in the near-shore bottom profile that can effectively enhance wave energy dissipation. Bedform geometry will regulate wave transformations and influence the sediment transport phenomenon. We begin with a historical review of the available literature. Next, a laboratory investigation of bedform geometry under regular and irregular surface gravity waves was conducted for two different depths in Towing Tank III at Davidson Laboratory. This wave tank facility provided an ideal opportunity for investigating bedform features for a flat bed and enabled the novel study of a sloped sediment bed. Our results provide new data that strengthens prior relationships and demonstrate that a sloped surface may be modeled in similar fashion to a flat sediment bed. These results also suggest that ripple dimensions may be independent of water depth and bottom orbital excursion amplitude (Ab) which is in contrast to the continental shelf under equilibrium conditions where ripples scale with Ab. The evaluation of wave tank dynamics was also conducted using an Acoustic Doppler Velocimeter (ADV) and surface wave data. Velocity measurements were performed using the ADV, and the wave records were measured using wave wire devices. The resulting data provided the basis for evaluating the hydrodynamics within the wave tank. Data analysis includes measurements of residual velocity and return flows that are inherent in a laboratory facility in the presence of propagating waves. The higher order harmonics that occur in laboratory facilities in the presence of monochromatic waves were evaluated as well. This information provides a new assessment of the hydrodynamics within Davidson Laboratory.
590 $a School code: 0733.
650 4 $a Engineering, Marine and Ocean. $3 1019064
650 4 $a Physical Oceanography. $3 1019163
690 $a 0547
690 $a 0415
710 2 0 $a Stevens Institute of Technology. $3 1019501
773 0 $t Dissertation Abstracts International $g 65-03B.
790 1 0 $a Bruno, Michael S., $e advisor
790 $a 0733
791 $a Ph.D.
792 $a 2004
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3127365