Technical Assistance Consultant’s Report
Project Number: 44167-012 December 2013
Bangladesh: Main River Flood and Bank Erosion Risk Management Program (Financed by the Japan Fund for Poverty Reduction)
Prepared by Northwest Hydraulic Consultants, Canada
In association with Resource Planning and Management Consultants Ltd., Bangladesh
For Bangladesh Water Development Board
This consultant’s report does not necessarily reflect the views of ADB or the Government concerned, and ADB and the Government cannot be held liable for its contents. (For project preparatory technical assistance: All the views expressed herein may not be incorporated into the proposed project’s design.
Government of the People's Republic of Bangladesh
Bangladesh Water Development Board
Project Preparatory Technical Assistance No. 8054 BAN
Main River Flood and Bank Erosion Risk Management Program
Final Report, Annex F Design Issues
September 2013
In association with
Resource Planning & Management Consultants Ltd. Asian Development Bank
Funded by the Japan Fund for Poverty Reduction
Government of the People’s Republic of Bangladesh Bangladesh Water Development Board
Project Preparatory Technical Assistance 8054 BAN Main River Flood and Bank Erosion Risk Management Program
Final Report, Annex F Design Issues
September 2013
PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
Document Status
Title: Designs Issues, Annex F
Annex F1 Geotechnical Investigations Principal Author: Ahsanul Jalil Khan Contributions: Annex F2 Technical Designs for Tranch‐1 Work Principal Author: Mukhles uz Zaman Contributions: Final version: August 2013
Document Development Draft Final June 2013 Final R1, 15 August 2013 Justify and page setup R2, 21 August 2013 Combined F1 & F2 two doc files and page setup R3, 28 August 2013 Inserted Two Appendix R4, 01 September 2013 Format cover page and header and footer R5, 22 September 2013 Checked for final print
R6, 30 September 2013 Added Annexures page
R7, 28 February 2014 Reprinted R6
Reviewed by:
Page ii September 2013 F1 Geotechnical Investigations
MAIN REPORT
ANNEXES
Annex A Priority Sub‐reach Selection & Sub‐reach Descriptions Annex A1 Priority Sub‐reach Selection Annex A2 Sub‐reach Description Annex B Background Data Annex B1 National Water Resources Database Annex B2 Socio‐economic Data Annex B3 Surveys and Field Visits Annex C Institutional and Financial Assessment Annex D Hydrology and Flood Modelling Annex E River and Charland Morphology and River Engineering Annex F Design Issues Annex F1 Geotechnical Investigations Annex F2 Technical Designs Annex G Economic Feasibility Annex G1 Project Cost Annex G2 Economic Assessment Annex H Implementation and Procurement Planning Annex I Social Gender Equity Strategy & Action Plan Annex J Environmental Impact Assessment Annex K Involuntary Resettlement Annex K1 Resettlement Framework Annex K2 Resettlement Plan
Page iii PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
Page iv September 2013
Asian Development Bank
Funded by the Japan Fund for Poverty Reduction
Government of the People’s Republic of Bangladesh Bangladesh Water Development Board
Project Preparatory Technical Assistance 8054 BAN Main River Flood and Bank Erosion Risk Management Program
Final Report, Annex F1 Geotechnical Investigations
September 2013
PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
Page vi September 2013 PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
Table of Contents
1 Introduction ...... 1 1.1 Background ...... 1 1.2 Geo‐technical Investigation ...... 2 2 Study sites with and Soil Data ...... 3 2.1 Borehole Location ...... 3 2.2 Field and Laboratory Tests ...... 7 2.3 Discussion of Results ...... 10 3 Sub‐Soil Profile ...... 11 4 Embankment stability: ...... 16 4.1 Introductory Remarks ...... 16 4.2 Stability analysis ...... 17 4.3 Settlement (of foundation soil beneath embankment) ...... 18 4.4 Check for seepage flow ...... 20 4.5 Check for horizontal sliding/pore water pressure within the embankment ...... 20 4.6 Stability against Earthquake/Check for liquefactions ...... 21 5 Riverbank Stability ...... 22 5.1 Data and calculation method ...... 22 5.1.1 Slope angles and Soil characteristics ...... 22 5.1.2 Calculation method ...... 23 5.2 Calculated Scenarios ...... 24 5.2.1 Existing Riverbank ...... 24 5.2.2 Designed river bank ...... 25 5.3 Summary and Conclusion ...... 28 6 Summery RBP ...... 29 6.1 General Geotechnical features ...... 29 6.2 Flood embankment stability ...... 29 6.3 Riverbank Protection ...... 29 7 References ...... 30
Page vii PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
List of Tables
Table 2‐1: Location, Bore‐hole depth & coordinate with ground and ground water elevations (Koizuri‐ Hurasagar section) ...... 3 Table 2‐2: Location, Bore‐hole depth & Coordinate with ground and ground water elevations (Chouhali‐ Nagarpur section) ...... 5 Table 2‐3: Location, Bore‐hole depth & Coordinate with ground and ground water elevations (Jafarganj‐ Bachamara section) ...... 5 Table 2‐4: Location, Bore‐hole depth & Coordinate with ground and ground water elevations (Enayetpur‐Koizuri section) ...... 6 Table 2‐5: KH‐4 Field and Corrected SPT (N’) ...... 8 Table 2‐6: KH‐ 9 Field and Corrected SPT (N’) ...... 8 Table 2‐7: KH‐40 Field and Corrected SPT (N’) ...... 8 Table 2‐8: JB‐2 Field and Corrected SPT (N’) ...... 8 Table 2‐9: CN‐10 Field and Corrected SPT (N’) ...... 9 Table 2‐10: CN‐13 Field and Corrected SPT (N’) ...... 9 Table 2‐11: EK‐5 Field and Corrected SPT (N’) ...... 9 Table 2‐12: EK‐10 Field and Corrected SPT (N’) ...... 10 Table 5‐1: Results of the calculation for existing Slopes ...... 24 Table 5‐2: Case 1‐ 19 m river bed ...... 26 Table 5‐3: Case 2‐ 39 m river bed ...... 26 Table 5‐4: Results of calculation for designed slopes ...... 27
Figures
Figure 1‐1 (a&b): Typical Sections of Proposed Flood Embankment ...... 2 Figure 2‐1: Satellite Image of Project Location ...... 6 Figure 2‐2: Satellite Image of Bore‐Hole Location ...... 7 Figure 3‐1: Bore Hole Log of Koizuri‐Hurashagar (KH) ...... 12 Figure 3‐2: Bore Hole Log of Enayetpur‐Koizuri (EK) ...... 13 Figure 3‐3: Bore Hole Log of Chauhali‐Nagarpur (CN) ...... 14 Figure 3‐4: Bore Hole Log of Jafarganj‐Bachamara (JB) ...... 15 Figure 5‐1: Profile of the cross sections at the Jamuna River right bank ...... 22 Figure 5‐2: Profile of the cross sections at the Jamuna River left bank ...... 22 Figure 5‐3: Safety factor for 35m slopes Figure 5‐4: Safety factor for 15 m slopes ...... 23 Figure 5‐5: Dimensions of existing slopes ...... 24 Figure 5‐6: Typical slip circles at an existing slope ...... 25 Figure 5‐7: Slope dimensions of designed slopes ...... 26 Figure 5‐8: Safety factor for 35m slopes Figure 5‐9: Safety factor form 15 slopes ...... 26 Figure 5‐10: Typical slip circles at a designed slope...... 27 Figure 6‐1: Comparison designed slope to existing river profile ...... 30
Page viii September 2013 F1 Geotechnical Investigations
1 Introduction
1.1 Background The Asian Development Bank (ADB) is undertaking a feasibility assessment of a flood and riverbank erosion risk management program covering parts of the main rivers of Bangladesh financed by the Japan Fund for Poverty Reduction (JFPR). The objective of the Main River Flood and Bank Erosion Risk Management Program (MRP) is to reduce the riverbank erosion and flood risks to the adjacent flood plains while maximizing economic activities in a sustainable and environmentally acceptable manner. Existing flood embankments dominantly fail from riverbank erosion, and as such the stabilization of the river pattern is a cornerstone of reducing the flood risk. The MRP builds on and extends the activities of the Jamuna‐Meghna River Erosion Mitigation Project (JMREMP) (ADB, 2002), implemented in different phases from January 2003 until June 2011. In addition, a similar project, the Assam Integrated Flood and Riverbank Erosion Risk Management Investment Project (AIFRERMIP; ADB, 2010) provides important insight into a number of relevant project elements and processes especially integrating disaster risk management measures related to flood and riverbank erosion risk management under the dictate of the Integrated Water Resources Management (IWRM) framework.
Subsequent to the preliminary assessment of geo‐technical aspects certain analytical evaluations have been made in order to obtain important and relevant geo‐technical parameters. The presentation of these parameters is basically on the assumption of fairly uniform sub soil strata and their properties and characteristics generally observed in the locality.
The main objective of present study is to formulate parameters for feasibility design of stability of the proposed flood embankment/levy/ dykes with some hydraulic structures having regulatory functions.
The report also includes study and design (stability) for River Bank protection measures separately in the later section.
The following basic data/ information were used as guide line for preliminary analysis of stability – (a) HFL – 100 years frequency in Brahmaputra Jamuna 50 years frequency in Boral and Hurasagar (b) Ground level along the alignment of the proposed embankment (c) Geo‐technical data – i) Bore holelogs ii) Field‐lab test results iii) BWDB data iv) Results of PIRDP of JMREMP investigation and analysis (d) Proposed options for typical x‐sections of embankment as shown in Figure 1.1.
The comments and observation received from BWDB design office were answered through a note on Design Criteria as Appendix‐IV and Comments and Observance as Appendix‐V in Annex F2.
Page 1 PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
Typical Cross section of Embankment ( Height- 5m)
Carriage width 1.5 Verge 1 Shoulder
1 2 3 0.75 1.5 5.5 Sand fill 1 3.5 2.5
Sand fill 60 cm excavated
15.0 3.2 3.0 10.0 8.75 39.95
Typical Cross section of Embankment ( Height- 5m)
Temporary Shelter 1.0 Carriage width 1.5 Verge 1 1 Shoulder 2 2 0.75 1.5 5.5 4.0 1 Sand fill 1 3.5 2 2.5
Sand fill 60 cm excavated
10.0 8.0 2.0 3.2 3.0 10.0 8.75 44.95
Figure 1‐1 (a&b): Typical Sections of Proposed Flood Embankment
1.2 Geo‐technical Investigation It is essential to understand the nature and behavior of the soil forming the river bank and also bed materials for the development of a bank protection work. In the present report relevant geo‐technical aspects are studied for analysis of flood embankment along the river bank, some distance apart from the existing bank. However, it is to be noted though that the anticipated failure modes of river bank are (a) erosion of soil due to wave and/or river current and sliding of slope due to instability induced by bed erosion or undercutting below water level. These modes of failure may take place where slope angle is not consistent with geo‐technical conditions prevailing at the site. A soil exploration program was therefore undertaken to investigate the sub soil condition at the selected project sites for main river flood embankment and bank erosion risk management program.
Accordingly, for the preliminary project formulation and feasibility study; a number of bore‐holes were explored through the Ground Water Hydrology Division of BWDB, during November 2011 to February 2012.
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2 Study sites with and Soil Data
2.1 Borehole Location At right bank of river Jamuna, 40 Bore Holes (BH) designated as KH‐1 to KH‐40, at Koizuri to Hurasagar and Bherakhola to Baghabari port in Sirajganj District. At right bank of river Jamuna, 14 BH designated as EK‐1 to EK‐14, from Enayetpur to Koizuri in Sirajganj district. At left bank of river Jamuna, 19 BH designated as CN‐1 to CN‐19 from Chouhali to Nagarpur, in Tangail District At left Bank of river Jamuna, 10 BH designated as JB‐1 to JB‐10 from Jafarganj to Bachamara in Manikganj District.
Depth of Bore‐hole, locations with co‐ordinates are shown in Table 2.1 and Bore Hole (BH) locations on Satellite image with co‐ordinates are shown in Figure 2.2.
Table 2‐1: Location, Bore‐hole depth & coordinate with ground and ground water elevations (Koizuri‐Hurasagar section) District Koizuri– Coordinates Upazila Depth Gr. Elv. GWT Hurasagar (KH) (m) PWD(m) PWD(m) KH1 N24°10´33.6´ E 89°41'28´´ Shajadpur 30 10.34 3.25 N673456 E468943 KH2 N24°10´21.8´´ E 89°41'17´´ Shajadpur 20 10.25 3.85 N673090 E468625 KH3 N24°10´04.0´ E 89°41'17´´ Shajadpur 30 10.16 2.87 N672550 E468627 KH4 N24°9´54.5´´ E 89°41'07´´ Shajadpur 20 10.12 2.998 N672252 E468333 KH5 N24°9´45.0´´ E 89°40'53´´ Shajadpur 30 10.35 3.28 N671963 E467922 KH6 N24°9´31.9´´ E 89°40'42´´ Shajadpur 20 9.94 2.64 N671558 E467628 KH7 N24°9´18.1´´ E 89°40'31´´ Shajadpur 30 10.17 3.28 N671136 E467305 KH8 N24°9´04.9´´ E89°40'23.5´´ Shajadpur 20 10.35 2.64
N670710 E467096 KH9 N24°8´52.6´´ E89°40'10.8´´ Shajadpur 30 10.15 3.28
Sirajganj N670348 E466732 KH10 N24°8´39.7´´ E89°40'0.7´´ Shajadpur 20 9.45 3.125 N669947 E466434 KH11 N24°8´26.9´´ E89°39'57.0´´ Shajadpur 30 10.27 2.64 N669550 E466428 KH12 N24°8´09.8´´ E 89°40'2.6´´ Shajadpur 20 10.25 2.69 N669044 E466490 KH13 N24°7´53.1´´ E89°39'58.3´´ Shajadpur 30 10.11 2.82 N668530 E466365 KH14 N24°6´37.6´´ E89°39'56.9´´ Shajadpur 20 10.05 2.52 N668043 E466328 KH15 N24°7´20.5´´ E89°39'55.9´´ Shajadpur 30 10.09 2.82 N667521 E466301 KH16 N24°7´03.7´´ E89°39'52.5´´ Shajadpur 20 9.81 2.52 N667010 E466215 KH17 N24°6´48.5´´ E89°39'46.9´´ Shajadpur 30 9.43 2.95
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District Koizuri– Coordinates Upazila Depth Gr. Elv. GWT Hurasagar (KH) (m) PWD(m) PWD(m) N666539 E466038 KH18 N24°6´33.0´´ E89°39'52.7´´ Shajadpur 20 10.03 2.69 N666063 E466191 KH19 N24°6´16.4´´ E89°39'01.6´´ Shajadpur 30 10.13 3.115 N665587 E466322 KH20 N24°6´01.5´´ E89°40'09.4´´ Shajadpur 20 10.06 2.69 N665098 E466464 KH21 N24°5´47.6´´ E89°40'14.0´´ Shajadpur 30 10.11 3.125 N664665 E466674 KH22 N24°5´33.3´´ E 89°40'.0´´ Shajadpur 20 10.07 2.62 N664196 E466808 KH23 N24°5´14.5´´ E89°40'12.0´´ Shajadpur 30 9.87 3.125 N663669 E466759 KH24 N24°5´04.0´´ E89°40'01.0´´ Shajadpur 20 9.68 2.69 N663313 E466428 KH25 N24°4´51.6´´ E89°39'55.4´´ Shajadpur 30 9.49 3.125 N662933 E466278 KH26 N24°4´36.3´´ E89°39'46.6´´ Shajadpur 20 9.56 2.515 N662476 E466023 KH27 N24°4´20.4´´ E89°39'39.4´´ Shajadpur 30 8.58 3.1 N663669 E466759 KH28 N24°4´30.4´´ E89°39'24.8´´ Shajadpur 20 7.72 3.4 N662300 E467148 KH29 N24°4´38.5´´ E89°39'15.1´´ Shajadpur 30 7.45 3.45 N662565 E465128 KH30 N24°4´45.6´´ E89°38'56.8´´ Shajadpur 20 7.51 2.49 N662763 E464624 KH31 N24°5´57.2´´ E89°38'33.7´´ Shajadpur 30 9.25 2.82 N663120 E464140 KH32 N24°5´08.1´´ E89°38'22.3´´ Shajadpur 20 7.95 3.1 N663461 E463652 KH33 N24°5´20.4´´ E89°38'04.0´´ Shajadpur 30 9.15 2.72 N663831 E463136 0KH34 N24°5´31.7´´ E89°37'46.9´´ Shajadpur 20 8.31 2.82 N664180 E462651 KH35 N24°5´44.2´´ E89°37'29.0´´ Shajadpur 30 9.05 3.15 N664568 E462148 KH36 N24°4´59.8´´ E89°37'11.5´´ Shajadpur 20 8.11 2.95 N665062 E461656 KH37 N24°4´09.2´´ E89°39'35.4´´ Shajadpur 40 9.07 3.18 N661642 E465689 KH38 N24°5´34.0´´ E89°39'58.5´´ Shajadpur 40 10.01 3.25 N662408 E466347 KH39 N24°5´01.2´´ E89°40'21.4´´ Shajadpur 40 10.12 3.10 N663225 E466960 KH40 N24°5´05.0´´ E89°40'26.1´´ Shajadpur 40 9.81 3.1 N664214 E465417
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Table 2‐2: Location, Bore‐hole depth & Coordinate with ground and ground water elevations (Chouhali‐Nagarpur section) District Chouhali‐ Coordinates Upazila Depth Gr. Elv. GWT Nagarpur (m) PWD(m) PWD(m) CN‐1 N24°18´07.3´´ E89°47´42.8´´ Omarpur 40 12.74 3.1 CN‐2 N24°17’38.2´´ E89°48´38.7´´ Norshinghopur 40 12.07 3.1 CN‐3 N24°17´08.9´’ E89°48´20.2´´ Dholabari 40 12.12 3.1 CN‐4 N24°16´44.2´´ E89°47´56.6´´ Kachua 40 11.63 3.1 CN‐5 N24°16´11.2´´ E89°47´51.4´´ Kachua 40 11.07 3.1 CN‐6 N24°15´42.5´´ E89°48´21.6´´ Degreehogra 40 12.14 3.1 CN‐7 N24°15´08.6´´ E89°48´19.5´´ Degreehogra 40 12.6 3.1 CN‐8 N24°14´32.2´´ E89°48´21.2´´ Alokdia 40 12.19 3.05 CN‐9 N24°14´00.0´´ E89°48´25.0´´ Alokdia 40 12.15 3.41
CN‐10 N24°13´29.4´´ E89°48´33.6´´ Ichapara 40 12.1 3.25
Tangail CN‐11 N24°12´56.6´´ E89°48´46.9´´ Rashidpur 40 12.07 3.56 CN‐12 N24°12’22.9´´ E89°48´55.3´´ Rashidpur 40 12 3.43 CN‐13 N24°12´14.2´´ E89°47´10.1´´ Chalchar 40 10.9 3.71 CN‐14 N24°11´40.7´´ E89°47´13.5´´ Misrogati 40 10.84 3.56 CN‐15 N24°11´07.6´´ E89°47´26.1´´ Dhalpakhla 40 11.11 3.25 CN‐16 N24°10´33.1´´ E89°47´33.1´´ Mahmoodpur 40 11 3.41 CN‐17 N24°09´58.8´´ E89°47´39.6´´ Mahmoodpur 40 11.02 3.1 CN‐18 N24°09´22.9´´ E89°47´42.7´´ Dolai 40 10.8 3.41 CN‐19 N24°08´45.7´´ E89°48´53.4´´ KhasKaulia 40 10.9 3.71
Table 2‐3: Location, Bore‐hole depth & Coordinate with ground and ground water elevations (Jafarganj‐ Bachamara section) Distric Jafarganj‐ Coordinates Upazila Depth Gr. Elv. GWT t Bachamara (m) PWD(m) PWD(m) JB1 N23°53´24.2´´ E89°45´42.3´´ Shibaloy 40 10 4.64 JB2 N23°53´58.4´´ E89°45´21.6´´ Shibaloy 40 9.2 3.71 JB3 N23°54´49´´ E89°45´43.2´´ Daulotpur 40 9 4.01 JB4 N23°55´40.2´´ E89°45´47.5´´ Daulotpur 40 8.5 3.76
JB5 N23°56´8.2´´ E89°46´4.1´´ Daulotpur 40 8.6 3.168 JB6 N23°57´8.4´´ E89°46´25.7´´ Daulotpur 40 10 3.84 Manikganj JB7 N23°57´56´´ E89°46´33.4´´ Daulotpur 40 8.8 3.86 JB8 N23°58´33.6´´ E89°46´33.8´´ Daulotpur 40 9.5 4.01 JB9 N23°59´17.4´´ E89°46´17.2´´ Daulotpur 40 10.2 4.47 JB10 N23°59´31.5´´ E89°45´29.8´´ Daulotpur 40 8 4.62
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Table 2‐4: Location, Bore‐hole depth & Coordinate with ground and ground water elevations (Enayetpur‐Koizuri section) Enayetpur‐ Gr. Elv. GWT District Co‐ordinates Upazila Depth Koizuri PWD(m) PWD(m) EK‐1 N24°11´28.2´´ E89°41´52.7´´ Enayetpur 40 10.35 3.48 N675136 E475667 EK‐2 N24°21´08.2´´ E89°42´02.7´´ Enayetpur 40 10.51 3.33 N676359 E469903 EK‐3 N24°12´43.9´´ E89°78´26.4´´ Enayetpur 40 10.19 3.61 N677461 E470567 EK‐4 N24°13´17.4´´ E89°71´48.8´´ Enayetpur 40 10.62 3.56 N678488 E471148 EK‐5 N24°13´58.7´´ E89°43´42.59´´ Enayetpur 40 10.81 3.56 N679750 E571495 EK‐6 N24°14´37.5´´ E89°43´20.3´´ Enayetpur 40 10.22 3.4045 N680954 E472095
EK‐7 N24°15´06.1´´ E89°44´47.9´´ Enayetpur 40 10.2 3.43 N682100 E473722 EK‐8 N24°15´14.8´´ E89°45´18.1´´ Enayetpur 40 10.83 3.1 Sirajganj N683100 E475306 EK‐9 N24°15´47.8´´ E89°45´14.1´´ Enayetpur 40 10.37 4.045 N684073 E475702 EK‐10 N24°16´19.2´´ E89°45´28.1´´ Enayetpur 40 10.45 3.15 N685034 E475907 EK‐11 N24°16´50.5´´ E89°45´35.2´´ Enayetpur 40 10.89 3.43 N686075 E476154 EK‐12 N24°17´24.2´´ E89°45´43.8´´ Enayetpur 40 11.17 3.56 N687047 E476074 EK‐13 N24°18´32.00´´ E89°45´34.8´´ Enayetpur 40 11.47 3.25 N688150 E475901 EK‐14 N24°19´21.8´´ E89°45´26.4´´ Enayetpur 40 11.64 3.125 N689701 E475667
Figure 2‐1: Satellite Image of Project Location
Page 6 September 2013 F1 Geotechnical Investigations
Figure 2‐2: Satellite Image of Bore‐Hole Location
2.2 Field and Laboratory Tests Sub‐soil investigation conducted in field presents bore‐hole logs with ground level (GL), Standard Penetration Tests (at every 1.5 meter) and stratification with lithological description. Laboratory test results include grain size distribution curves, atterberg limit tests, consolidation parameters, natural moisture contents, specific gravity, density test with OMC maximum dry density, unconfined compression (U.C) tests and unconsolidated undrained (U.U) triaxial compression tests. Very brief analysis has been made on the result of the above soil investigation reports and some salient feature are presented in Tables 2.5 ‐ 2.12. Observation and findings of previous investigations and study conducted under JMREMP in 1992, 1993 and also during 2001 and 2006 were reviewed in the present study.
Page 7 PPTA 8054: Main River Flood and Bank Erosion Risk Management Program
Soil constituents (with some parameters)
Table 2‐5: KH‐4 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 2 70 30 M+FS 0.045 0.009 5 58 42 CL/ML+FS 0.06 0.01 7.5 7 93 FS 0.14 0.008 9 7 93 FS 0.14 0.008 12.2 8 92 FS 0.135 0.09 15 8 92 FS 0.149 0.074 18.3 4 96 FS 0.147 0.085
Table 2‐6: KH‐9 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 2 66 34.1 SANDYSILT +NP+ML 0.04 0.005 3 56 44 VFS+MC+NP 0.08 0.006 7.5 11 89 FS 0.14 0.065 10 14 86 FS 0.125 0.060 15 6 94 FS 0.13 0.090 18.3 8 92 FS 0.125 0.08 23 6 94 FS 0.140 0.075 30 4 96 FS 0.149 0.090
Table 2‐7: KH‐40 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 2 88 12 CL+ML 0.01 0.0015 3 68 32 ML+CL 0.045 0.0092 5 48 52 ML+FS 0.08 0.0175 4 18 82 FS 0.10 0.04 11 16 84 FS 0.125 0.05 15 15 85 FS 0.125 0.06 23 8 92 FS 0.140 0.08 30 16 84 FS 0.12 0.06 40 2 98 FS 0.149 0.092
Table 2‐8: JB‐2 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 1.5 44 56 0.08 3 42 58 CH 0.085 5 30 70 FS+M 0.095 6 12.1 89 FS 0.15 6.7 14 86 FS 0.135 10 9 91 FS 0.163 24.16 2.66 12 9 91 FS 0.155 24.96 1.66 15 10 90 FS 0.155 18.6 9 91 FS 0.155 23 9 91 FS 0.155 26 9.5 90.5 FS 0.163 30 12 88 FS 0.149 36 12 88 FS 0.155
Page 8 September 2013 F1 Geotechnical Investigations
Table 2‐9: CN‐10 Field and Corrected SPT (N’)
Depth( m) C(%) M (%) S (%) Soil Types NMC 2 75 25 ML(NP) 0.045 0.01 3‐4 76 24 ML(NP) 0.037 0.007 5 72 28 ML+SP 0.04 0.01 20.43 2.665 6.5 76 24 ML+SP 0.045 0.01 12.1 2.663 10 14 36 ML 0.155 0.06 8 78 22 ML 0.0455 0.009 12.5 70 30 FS 0.052 0.009 15 10 90 FS 0.18 0.08 20 30 70 FS 0.12 0.025 23 28 72 FS 0.125 0.03 26 10 90 FS 0.18 0.075 30 9 91 FS 0.175 0.08 35 8 92 FS 0.18 0.085
Table 2‐10: CN‐13 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 2 74 26 ML 0.04 0.009 3.5 72 28 ML(NP) 0.052 0.012 4.5 76 24 ML 0.046 0.009 6.5 30 70 FS 0.13 0.025 10 25 75 FS 0.125 0.04 12 24 76 FS 0.125 0.04 15 24 76 FS 0.130 0.05 20 16 84 FS 0.12 0.055 25 4 96 FS 0.21 0.12 27 6 94 FS(SP) 0.2 0.10 30 18 82 FS(SP) 0.125 0.05 35 16 84 FS(SP) 0.14 0.05 38 18 82 FS(SP) 0.135 0.055
Table 2‐11: EK‐5 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 1.5 47 53 FS+M+NP 0.08 0.025 3 66 34 ML+FS 0.058 0.018 5 66 34 M+FS 0.058 0.018 6.5 14 86 FS 0.156 0.06 8 12 88 FS 0.152 0.10 10 10 90 FS 0.149 0.07 11 4 96 FS 0.14 0.092 12.5 6 94 FS 0.17 0.088 13.7 4 96 FS 0.125 0.088 15 2 98 FS 0.135 0.092 18.5 4 96 FS 0.149 0.085 22 6 94 FS 0.125 0.08 24.7 8 92 FS 0.155 0.085 30 2 98 FS 0.152 0.10 35 2 98 FS 0.149 0.093 38 2 98 FS 0.155 0.095 40 2 98 FS 0.149 0.095
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Table 2‐12: EK‐10 Field and Corrected SPT (N’)
Depth (m) C (%) M (%) S (%) Soil Types NMC 1.5 8 92 FS 0.22 0.09 4.5 2 98 FS 0.149 0.092 10.5 2 98 FS 0.175 0.10 12.5 6 94 FS 0.156 0.088 15 4 96 FS 0.149 0.095 20 4 96 FS 0.152 0.088 25 6 94 FS 0.154 0.085 30 4 96 FS 0.149 0.09 35 6 94 FS 0.140 0.083 40 4 94 FS 0.149 0.09
NOTE: C= Clay minerals M= Silt S= Sand VFC= Very fine sand FS= Fine sand NP= Non‐Plastic ML= Silt low plastic CL= Clay low Plastic CH= Clay High Plastic MH= Silt High Plastic
2.3 Discussion of Results The BWDB undertook fairly comprehensive sub‐soil investigation all along the proposed alignment for flood embankment and river bank protection works. The Geotechnical investigation performed by BWDB will time bound program (carried and hurriedly) resulting in some uncertainties about the accuracy of the findings. But as mentioned earlier, the sub soil composition in the project location is generally uniform. However, subsoil data obtained and used in the analysis appear to be reasonably consistent with the past reports and results. Further, it is expected the factor of safety provided would compensate for local and general uncertainties
Further due to large distances between the bore‐holes (300m to about 400m), it may be worthwhile to undertake a limited number of additional bore‐holes before finalizing the design of embankment for some specific locations only.
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3 Sub‐Soil Profile
Figure 2.2 shows the Bore‐hole from 4 (four) locations referred earlier. Detailed bore‐hole logs are shown in Figure 3.1‐3.4. In each location (KH, EK, CN, JB) It is seen that the upper part of the soil (i.e. generally on average above RL +4.00 m PWD) is mostly dsilt an clay (CL, ML) type with varying quantities of fine to very fine sand (Non‐cohesive). This strata is underlain by very fine to fine sand (non‐cohesive) with little to trace silt and mica. The above feature is also evident in Table 2‐1 from the plot of and against depth for different Bore‐holes (Presented in Tables 2.5‐2.12). The SPT"N" Values for different Boreholes with corrected “ ” values are presented in Appendix 2, Tables A2.1 to A2.4.
The following observation can be highlighted:
The sub‐surface soil formation consists of two layer system.
In general in all four section, the upper layer consists of fine grained soil of low to inter‐mediate plasticity with few exceptions where in it is referred to as plastic, semi‐plastic or even non‐ plastic (upto above EL+4 to+5m PWD). Broadly Classified as CL‐ML type soil
The lower part (i.e. below +4 to +5m PWD) mainly consists of very fine to fine to medium grained sands upto depth of exploration. Very thin films of mica mineral in traces were also encountered at varying depths.
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Figure 3‐1: Bore Hole Log of Koizuri‐Hurasagar (KH)
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Figure 3‐2: Bore Hole Log of Enayetpur‐Koizuri (EK)
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Figure 3‐3: Bore Hole Log of Chouhali‐Nagarpur (CN)
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Figure 3‐4: Bore Hole Log of Jafarganj‐Bachamara (JB)
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4 Embankment stability
4.1 Introductory Remarks The project areas are located in the delta of large rivers the Jamuna, a part of Brahmaputra river system, and the Padma. The terrain is formed by the river sediments of the flood plains. The channels frequently shift sideways due to erosion of the river banks or concentrate their discharge in other river channels. The river sediments consist of finely grained sand of medium compactness. The sand in all the project sites originate from the Himalayan Mountains and therefore consist of minerals, quartz, feldspar, rock fragments, trace heavy mineral and mica.
The amount of mica varies at different depths, which are rather inconsistent. Previous documents and study reports in the same region suggest mica content from 30% to 50% in some places. The recent BUET studies however put the figure between 7% to 11%, which seems to be reasonable [Special Report‐22 (Geotechnical) of Jamuna‐Meghna River Erosion Mitigation Project, Part‐B, November 2006]. These river sediments are more or less horizontally layered with a very small inclination of layers in downstream direction. The mica minerals and the others particles have a more stocky shape. The sedimentation of quartz, feldspar and heavy minerals is much faster than mica minerals. It is observed from previous studies; the mica minerals form a very thin film of impermeable layer above more compact minerals.
A generalized summary of drilling at the project locations show a upper clay‐silt or silt‐clay layers referred to in the this report as CL‐ML (often found to be CH‐MH) which consists of silt clay / clayey silt with low to medium plasticity. Below the upper clayey layer fine grained and poorly graded sand, referred to as SP/SM or FS, sometimes very fine sand, VFS of medium compactness are present. The sand strata has a general trend of mild increase in density from medium to dense becoming very dense at depth around 30m and below.(As evident from BH‐Logs showing SPT plots in Figure 3.1‐3.4.
Geo‐technical slope failure in clay is commonly calculated by circular failure planes. Which means during failure rotation takes planes. Sand, however, shows more ors les straight failure planes; therefore translation may take place in case of failure.
Due to cohesion, clay is able to stand vertically up to a certain depth, where as pure sand without cementation will not remain stable under normal condition. In a state of low humidity (slightly moist) the sand yma have a small cohesion due to capillary action which disappears when it is dry or saturation is above 70% or so. This apparent cohesion can therefore be considered for calculation of an existing slope, but surely not for new construction. It may be noted that this part of the report deals with new flood protection embankment fairly close to existing river banks. In the present study with regular flooding of the terrain apparent cohesion may be introduced in stability analysis. At lower levels (higher depth), due to lithification of salts cementation may result in a low effective cohesion.
The clay layer on the surface of the terrain is considered sufficiently resistant. In view of its effective shear strength (without any reduction factor) the clay is able to stand vertically up‐to a certain height (around 4m or so). It is to emphasize though that in the case of slope failure, the excess of the stability of clay cannot be transferred or related to improve the stability of the sand layer below.
The survey carried during previous study observed that the slopes for the upper clay layer was fairly steep and derived magnitude of unconfined compression strength was found to be Cu=30 ‐40 kpa. BUET study conducted during 2004 also appears to confirm this value.
The observed slope inclination at river in sand is found to be 1:2.5‐1:3 for about 50% of the project area which is expected with limit equilibrium condition. The angle of internal friction, which is the shear strength of sand in these case, are 28 ‐ 30 with very low effective cohesion estimated at c=2‐4 kpa.
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In view of the uncertainties associated with the effect of cohesion at this stage, it is ignored in the stability analysis as shown in the later illustrations. The lower strata below the fine grained clay silt formulation predominantly consist of sand (fine sand with little to trace silt) and occasional Mica. eTh layer generally is of medium density as evident from interpretation of standard penetration 'N' test values. There is mild trend of increase in density with increase in depth. Further below the density is found to be medium dense to dense becoming very dense usually below 30‐35m depth of exploration. The above observation appears to agree favorably with BUET Report including earlier reports of JMREMP and FAP (Halcrow Feasibility) Studies and those of Jamuna Bridge etc.
4.2 Stability Analysis On the basis of above information and geotechnical investigation carried out by BWDB, some preliminary stability analysis may be made for the proposed flood protection embankment and bank erosion. The slope protection and erosion control of the vulnerable river bank is not considered here and are addressed separately at a later stage.
For the purpose of analysis the following assumptions are made: Assume dredged fill material for embankment construction Embankment height 4m‐ 6m (i.e. 5m on average) Compacted fine sand with angle of internal friction =28 to 30_use 30 Embankment slope: 1:3 and 1:2.5 A factor safely fs≥ 1.4 has been considered as standard in line with previous project designs for river bank stability (PIRDP).
Assume: Dredged soil from river bed River bed material mainly fine sand/ very fine sand with silt/ silty fine sand/ silt with very fine sand occasional at shallow depths. The Feature of predominant fine particles is observed at shallow depths (5‐7m). Compacted fill material have angle of internal friction φ=28‐30 Slope angle , i.e. slope is 1:3, 1:2.5 and 1:2, considered for trial.
Under normal conditions: Factor of safety (f) against failure tan f tan , Dredged fill soil f = FS = Factor of Safety Ø 28° min. to 30°, use 30° β 5m
For Ø 28° For Ø 30° Slope 1:3, Slope 1:3, f = tan 28°/ tan 18.43° = 0.532/0.33= 1.6 f = tan 30°/tan 18.43° = 0.577/0.333 = 1.7 Slope 1:2.5, Slope 1:2.5, f = tan 28°/tan 21.80° = 0.532/0.40 = 1.33 f = tan 30°/tan 21.80° = 0.577/0.40 = 1.44 Slope 1:2, f = tan 30°/ tan 26.57° = 0.577/0.50 = 1.15
Under Submerged Condition
tan .0*8 577 f sub .0 778 .1 25 tan 18 .0* 33 sand
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