Scour Analysis at Seawall in Salurang, Sangihe Islands Regency, North Sulawesi

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PROCEEDING OF 3 RD INTERNATIONAL CONFERENCE ON RESEARCH, IMPLEMENTATION AND EDUCATION OF MATHEMATICS AND SCIENCE YOGYAKARTA, 16 17 MAY 2016 M 04 Scour Analysis at Seawall in Salurang, Sangihe Islands Regency, North Sulawesi Eunike Irene Kumaseh 1, Suntoyo 2, Muh.Zikra 3 1, 2,3 Department of Ocean Engineering, Faculty of Marine Technology, Institut Teknologi Sepuluh Nopember, Surabaya - Indonesia eunikekumaseh@gmx.com Abstract. Sangihe Islands Regency is one of the outermost regions of the unitary Republic of Indonesia. The area is dominated by coastal areas. Thus, many coastal structures protection built to guard the coastal areas from the threat of big waves. Local scour is the erosion of the basis on a particular part of a building coast. If it occurs continously, it could lead to instability of the structure or structural failure. The research takes a case study on scouring at Seawall in Salurang, Sangihe Islands Regency, North Sulawesi. This study aims to determine dominant factor of scouring and predict the maximum scour depth and scour length at seawall by using Van Rijn method (2013) which is one method of numerical calculation. The method is expected to provide the right solution for handling a scouring at coastal structures in this area. The right method to predict maximum scour depth in Salurang, Sangihe Islands regency is the scour method near the tip of wall-type or rubble-mound-type structure due to waves (plus weak currents <0.3 m/s). Scour due to combination of waves and currents. The maximum scour depth value is 0.36 m and the scour length is 3.6 m. The local government can protect the coastal structure by providing stone mound at the toe based on the calculation of the maximum scour depth. Keywords: Maximum scour depth, seawall, Van Rijn method, Sangihe Islands Regency I. INTRODUCTION Sangihe Islands Regency is an integral part of the capital city of North Sulawesi Tahuna. Located approximately 142 Nautical Miles from the capital of North Sulawesi, Manado, located between 2 4'13 "- 4 44 '22" North Latitude and 125 9' 28 "- 125 56 '57" East, located between the Sulawesi islands and Mindanao (Republic of the Philippines), so the Sangihe Islands Regency can be categorized as "Frontier". The total area of Sangihe Islands Regency amounted to 736.98 km2 [1]. As a coastal region, this region, many built of coastal protection structures to prevent the influence of big waves. Seawall was built in Salurang village in 2003 with a length of 471.2 m, a width of 1 m and a height of 4 m. However, the scouring which caused by damage to some parts of the structure will occur in the local seawall few years later. Sumer, et al. (2001) has conducted research on scouring the various types of coastal structures and scour depth development model with physical and numerical modeling [5]. El-bisy (2006) has studied on the seawalls and predict scour using neural network models (ANNs) [3]. This study will predict the maximum scour depth on the seawall in Kampung Salurang using Van Rijn method (2013) [9]. Thus, is expected to provide the right solution for protection against scouring. And, the proper handling of coastal protection. Scour will occur anywhere the hydrodynamic shear stresses on the bottom are high enough to initiate sediment transport. Clear water scour occurs when bottom shear stresses are high only in a localized portion of the bed; outside the local region sediment is not moving. This occurs mostly in uniform, steady flow situations. In live bed scour, bottom shear stresses over the entire bed exceed the level for incipient motion with locally higher shear stresses where greater scour occurs. An equilibrium is reached when the volume of sediment being removed from the scour hole is exactly equal to sediment being deposited in its place. Understanding the physical processes involved in scour is difficult because M - 21

ISBN 978-602-74529-0-9 the shear stresses responsible for scour are developed by waves, currents, or combined waves and currents, that usually are heavily influenced by the presence of a coastal structure. Because of the distinct influence coastal structures exert on the hydrodynamics, structural aspects such as geometry, location, and physical characteristics (roughness, permeability, etc.) impact the scour process. Therefore, modifying some physical characteristic of a structure may reduce scour potential. [2] II. METHODS A. Refraction Analysis To get a value of wave height at structure, it is necessary to analyze the refraction, by some calculations below. (m) [wave length at deep water] (1) (m/s) [celerity at deep water] (2) (m) [wave length] (3) (m) [celerity] (4) [a = incident wave angle] (5) [refraction coefficient] (6) [shoaling coefficient] (7) (m) [wave height] [10] (8) B. Van Rijn Method To predict maximum scour depth, used the formulas below. #1 Scour near toe of wall-type or rubble-mound-type structures due to waves Scour s formula for Wall-type structure a. SPM, 1984 (9) b. Fowler, 1992 c. SATO, 1968 d. Yokoyama, 2002 e. Xie, 1981 Scour s formula for Rubble-mound-type structure Scour length is assumed to be scour depth of wall type structures. #2 Scour near tip of wall-type and rubble-mound type structures due to waves (plus weak current < 0.3 m/s) Scour s formula for Wall-type structure Sumer, 1997 Maximum value of: (18) (10) (11) (12) (13) (14) (15) (16) (17) ; (19) and (20) Scour s formula for Rubble-mound-type structure a. Sumer, 1997 Maximum value between M - 22

PROCEEDING OF 3 RD INTERNATIONAL CONFERENCE ON RESEARCH, IMPLEMENTATION AND EDUCATION OF MATHEMATICS AND SCIENCE YOGYAKARTA, 16 17 MAY 2016 And, (23) b. Field Data Japan, USA (24) (25) (26) #3 Scour near tip of wall-type and rubble-mound type structures due to relatively strong current (> 0.3 m/s) plus waves Generally, for scour length = 10 x Scour depth (29) Where = depth at toe exclude scour, = maximum scour depth, = safety factor, = peak wave period, = local wave height at toe, = Keulegan-Carpenter Number, = width of structure, = wave length, = significant wave height, = offshore significant wave height. And the mathematical formula for computing correlation coefficient = is: (21) (22) (27) (28), (30) where is the number of pairs of data. The value of is that. The and signs are used for positive linear correlations and negative linear correlations, respectively. The coefficient of determination, or, is useful because it gives the proportion of the variance (fluctuation) of one variable that is predictable from the other variable. The coefficient of determination is the ratio of the explained variation to the total variation. The coefficient of determination is such that, and denotes the strength of the linear association between and. The coefficient of determination represents the percent of the data that is closest to the line of best fit. III. RESULTS AND DISCUSSION The results of measurement and prediction for the maximum scour depth were shown in Tables 1-4. The comparison was given in Figure 1-3. Results of Measurement TABEL 1. SCOUR DEPTH BY MEASUREMENT 1 0.6 6 1.79 0.64 6.4 1.95 0.37 3.7 Results of Prediction a. Scour near toe of wall-type or rubble mound-type structure due to waves TABEL 2. MAXIMUM SCOUR DEPTH DUE TO WAVES 1 1.05 10.5 1.79 1.27 12.7 1.95 1.31 13.1 M - 23

ISBN 978-602-74529-0-9 FIGURE 1. COMPARISON BETWEEN PREDICTION AND MEASUREMENT DUE TO WAVES Based on the comparison between measurement and prediction have a coefficient correlation = = 0.4. And. It means that the prediction not accurately because the value of closest to. b. Scour near tip of wall-type or rubble-mound-type structure due to waves (plus weak currents <0.3 m/s) TABEL 3. MAXIMUM SCOUR DEPTH DUE TO WAVES PLUS WEAK CURRENT 1 0.3 3 1.79 0.36 3.6 1.95 0.35 3.5 FIGURE 2. COMPARISON BETWEEN PREDICTION AND MEASUREMENT DUE TO WAVES PLUS WEAK CURRENT Based on the comparison between prediction and measurement have a coefficient correlation = 0.9. And. It means that the prediction very accurately because the value of closest to. M - 24

PROCEEDING OF 3 RD INTERNATIONAL CONFERENCE ON RESEARCH, IMPLEMENTATION AND EDUCATION OF MATHEMATICS AND SCIENCE YOGYAKARTA, 16 17 MAY 2016 c. Scour near tip of wall-type or rubble-mound-type structure due to relatively strong current (>0.3 m/s) plus waves. TABEL 4. MAXIMUM SCOUR DEPTH DUE TO WAVES PLUS STRONG CURRENT 1 3.75 37.5 1.79 6.36 63.6 1.95 6.85 68.5 FIGURE 3. COMPARISON BETWEEN PREDICTED AND MEASUREMENT DUE TO WAVES PLUS STRONG CURRENT Based on the comparison between prediction and measurement have a coefficient correlation = 0.4. And. It means that the prediction not accurately because the value of closest to. From the results of comparison above, it can be seen that closest to 1 was on scour method calculation near the tip of wall-type or rubble-mound-type structure due to waves (plus weak currents <0.3 m/s ). Scour due to combination of waves and currents. Thus, it can be said that the right method to be used in the calculation of scouring in the Salurang village, Sangihe Islands Regency is a scour method calculation near the tip of wall-type or rubble-mound-type structure due to waves (plus weak currents <0.3 m / s) with a maximum scour depth is 0.36 m and scour length is 3.6 m. IV. CONCLUSION The right method to predict maximum scour depth in Salurang, Sangihe Islands regency is the scour method near the tip of wall-type or rubble-mound-type structure due to waves (plus weak currents <0.3 m/s). Scour due to combination of waves and currents. The maximum scour depth value is 0.36 m and the scour length is 3.6 m. The local government can protect the coastal structure by providing stone mound at the toe based on the calculation of the maximum scour depth. ACKNOWLEDGEMENT Thank you for Mr. Suntoyo and Mr. Zikra for guide the first author, for support from my classmate, Laboratory of post graduate Faculty of Marine Technology, and for everybody who completing this study. Hopefully this article can be useful. M - 25

ISBN 978-602-74529-0-9 REFERENCES [1] Kepulauan Sangihe dalam Angka, Badan Pusat Statistik Kabupaten Kepulauan Sangihe, 2014. [2] Coastal Engineering Manual, Fundamental of Design, US Army Corps of Engineers, 2001, VI-5-231-243. [3] El-Bisy, Mousa S., Bed changes at toe of inclined seawalls, Ocean Engineering, vol. 34, 2006, 510-517. [4] Sumer, B. M., Whitehouse, R. J. S., dan Torum, A., Scour around coastal structures: a summary of recent research, Coastal Engineering, vol. 44, 2001, 153-190. [5] Sumer, B. M dan Fredsoe, J., The Mechanics of Scour in the Marine Environment, Volume 17, World Scientific Publishing Co. Pte. Ltd., Singapore, 2002, 399-419. [6] Van Rijn, Leo C., Unified View of Sediment Transport by Currents and Waves. I : Initation of Motion, Bed Roughness, and Bed Load Transport, Journal of Hydraulic Engineering, ASCE, 2007, 649-667. [7] Van Rijn, L. C. (2013), Local Scour Near Structures www.leovanrijn-sediment.com, 2013, 1-31. [8] Triatmodjo, B., Teknik Pantai, Beta Offset, Yogyakarta, 1999, 67-94. M - 26