IS 13365 Part 31997AI Search Enabled✦ AI Generated

The quantitative classification system of rock mass-Guidelines, Part 3: Determination of slope mass rating

IS 13365 Part 3: 1997 provides guidelines for determining the Slope Mass Rating (SMR), a quantitative measure used to assess the stability of rock slopes. It builds on the Rock Mass Rating (RMR) system by incorporating adjustment factors related to joint orientation, failure modes, groundwater conditions, and excavation methods. This standard is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in slope stability analysis, landslide hazard zonation, and design of rock slope support systems in hilly and rocky terrains.

11Sections
37Clauses Indexed
AI Search Ready
1997Edition
Rock MechanicsCategory
Alternative search terms: IS 13365 Part 3 PDF, IS 13365 Part 3 pdf free download, IS 13365 Part 3 free download pdf, IS13365Part3 PDF, IS-13365-Part-3 PDF, IS 13365 Part 3 1997 PDF, IS 13365 Part 3:1997 PDF, IS 13365 Part 3-1997 PDF, IS 13365 Part 3 (1997) PDF, IS 13365 Part 3 1997 edition PDF, IS 13365 Part 3 edition 1997 PDF

What This Standard Covers

IS 13365 Part 3: 1997 provides guidelines for determining the Slope Mass Rating (SMR), a quantitative measure used to assess the stability of rock slopes. It builds on the Rock Mass Rating (RMR) system by incorporating adjustment factors related to joint orientation, failure modes, groundwater conditions, and excavation methods. This standard is essential for geotechnical engineers, rock mechanics specialists, and civil engineers involved in slope stability analysis, landslide hazard zonation, and design of rock slope support systems in hilly and rocky terrains.

Who Uses This Standard

  • Geotechnical Engineers
  • Rock Mechanics Specialists
  • Civil Engineers
  • Mining Engineers
  • Geologists
  • Slope Stability Analysts
  • Construction Project Managers

Key Topics Covered

Rock Mass Rating (RMR) basics
Slope Mass Rating (SMR) calculation
Adjustment factors for joint orientation
Failure modes: planar, wedge, toppling
Groundwater influence on slope stability
Methods of slope excavation and their impact
Field data collection and stereonet analysis
Classification of slope stability based on SMR
Remedial measures for unstable slopes
Safe cut slope angle determination
Use of IS referenced standards for rock properties
Application in landslide hazard zonation

Table of Contents

1Scope

IS 13365 Part 3: Scope Summary

  • Scope: Part 3 focuses on the Determination of Slope Mass Rating (SMR), a quantitative classification system for rock masses related to slope stability assessment.

  • Purpose: To provide guidelines for evaluating rock mass conditions influencing slope design and stability.

  • Key Concept: SMR modifies the Rock Mass Rating (RMR) based on slope orientation and discontinuity characteristics.


Key Formula: Slope Mass Rating (SMR)

[ \text{SMR} = RMR_b + F_1 + F_2 + F_3 ]

  • RMR_b: Basic Rock Mass Rating (from IS 13365 Part 1)
  • F1, F2, F3: Adjustment factors based on:
    • F1: Orientation of discontinuities relative to slope face
    • F2: Parallelism between discontinuities and slope face
    • F3: Excavation method and slope geometry

Typical Adjustment Factors (Example):

FactorDescriptionValue Range
F1Discontinuity-slope face angle-15 to 0
F2Discontinuity dip direction-20 to 0
F3Excavation method and slope shape-25 to +10

Notes:

  • Use IS 2:1960 for rounding final numerical values.
  • SMR helps in designing stable rock slopes by quantifying rock mass quality and structural orientation.
flowchart LR
    RMR_b --> SMR
    F1 --> SMR
    F2 --> SMR
    F3 --> SMR
    SMR --> Slope_Stability_Design

For detailed tables and factor values, refer to IS 13365 Part 3 text.

2Estimation of Rock Mass Rating (RMR basic)

Estimation of Rock Mass Rating (RMR basic) - IS 13365 Part 3

RMR basic is the sum of ratings from five key parameters (Clause 3.1, Table 1):

ParameterReference Standard
1. Uniaxial compressive strengthIS 8764
2. Rock Quality Designation (RQD)IS 11315 (Part 11)
3. Spacing of discontinuitiesIS 11315 (Part 2)
4. Condition of discontinuitiesIS 11315 (Part 4)
5. Groundwater conditionsIS 11315 (Part 8)

Slope Mass Rating (SMR) Calculation (Clause 3.4):

[ \boxed{ \text{SMR} = \text{RMR}_{basic} + (F_1 \times F_2 \times F_3) + F_4 } ]

  • F1, F2, F3: Adjustment factors based on discontinuity orientation relative to slope (Table 2).
  • F4: Adjustment for excavation method (Table 3).

Adjustment Factors for Joints (Table 2 Summary):

FactorDescriptionRating Range (Example)
F1Parallelism between slope & joint0.15 (Very favourable) to 1.00 (Very unfavourable)
F2Dip of discontinuity0.15 to 1.00
F3Relation between dip of joint & slope0 to -60 (negative values reduce SMR)

Excavation Method Adjustment (F4) - Table 3:

MethodF4 Rating
Natural slope+15
Presplitting+10
Smooth blasting+8
Blasting or mechanical0
Deficient blasting-8

Stability Classification Based on SMR (Clause 3.4):

SMR RangeStability
81 - 100Fully
3Determination of Failure Modes in Rock Slopes

Determination of Failure Modes in Rock Slopes (IS 13365 Part 3)

Key Points:

  • Failure modes depend on geological discontinuities; main types are Plane Failure, Wedge Failure, and Toppling Failure.
  • Field Data Collection: 100-500 discontinuity readings plotted on an equal area stereonet to identify pole concentration maximas indicating failure mode (Fig. 1).

Failure Mode Identification

Failure ModeDescriptionKey Condition
Plane FailureSliding along a single discontinuity planeDiscontinuity dip < slope dip
Wedge FailureSliding along intersection of two discontinuitiesIntersection line plunge < slope inclination
Toppling FailureRotation about a hinge formed by steeply dipping jointsSteeply dipping discontinuities

Rating System for Rock Mass (RMRbasic) [Table 1]

ParameterRangesRating
Strength of intact rock>10 MPa to <1 MPa15 to 0
Drill core quality (ROD)90-100% to <25%20 to 3
Spacing of discontinuities>2m to <60mm20 to 5
Ground water conditionDry to Flowing15 to 0

Adjustment Ratings for Joints (F1, F2, F3) [Table 2]

FactorParameterVery FavorableFavorableFairUnfavorableVery Unfavorable
F1Parallelism (aj - as)>30°30°-20°20°-10°10°-5°<5°
F2Dip of discontinuity<20°20°-30°30°-35°35°-45°>45°
F3Dip difference (Bj - Bs)>10°10°-0°0° to -10°<-10°

Adjustment for Excavation Method (F4) [Table 3]

| Method

4Estimation of Slope Mass Rating (SMR)

Estimation of Slope Mass Rating (SMR) as per IS 13365 Part 3


Key Formula:

[ \boxed{ \text{SMR} = \text{RMR}_{basic} + (F_1 \times F_2 \times F_3) + F_4 } ]

  • RMR_basic: Basic Rock Mass Rating (from IS 13365 Part 1)
  • F1, F2, F3, F4: Adjustment factors based on slope geometry and discontinuity characteristics

Stability Classification (Table 4):

SMR RangeStability Class
81 - 100Fully Stable
61 - 80Stable
41 - 60Partially Stable
21 - 40Unstable
< 20Very Unstable

Notes:

  • F1, F2, F3 are multiplicative factors modifying RMR_basic based on orientation of discontinuities relative to slope face.
  • F4 is an additive correction factor for special conditions (e.g., groundwater, weathering).
  • SMR is widely used for landslide hazard zonation and slope stability assessment in rock masses.

If you need detailed values or charts for F1, F2, F3, and F4, please specify.

5Adjustment Ratings for Joints and Excavation Methods

Key Formulas & Tables from IS 13365 Part 3: Adjustment Ratings for Joints & Excavation Methods


1. Slope Mass Rating (SMR) Formula:

[ \boxed{ \text{SMR} = \text{RMR}_{basic} + (F_1 \times F_2 \times F_3) + F_4 } ]

  • RMRbasic: Rock Mass Rating from 5 parameters (strength, RQD, spacing, condition, groundwater).
  • (F_1, F_2, F_3): Adjustment factors based on joint-slope geometry.
  • (F_4): Adjustment for excavation method.

2. Adjustment Factors for Joints (Table 2):

CaseParameterVery FavourableFavourableFairUnfavourableVery Unfavourable
P (Plane failure)(F_1) (angle (a_j - a_s))>30°30°-20°20°-10°10°-5°<5°
Values0.150.400.700.851.00
P(F_2) (dip (B_j))<20°20°-30°30°-35°35°-45°>45°
Values0.150.400.700.851.00
P(F_3) (dip difference (B_j - B_s))>10°10°-0°0° to -10°<-10°
Values0-6-25-50-60
  • (a_s): slope dip direction
  • (a_j): joint dip direction
  • (B_j): joint dip
  • (B_s): slope dip

3. Adjustment Rating for Excavation Methods (Table 3):

| Method | (

6Collection of Field Data and Stereonet Analysis

IS 13365 Part 3: Collection of Field Data & Stereonet Analysis

1. Collection of Field Data (Clause 3.2.4)

  • Take 100 to 500 readings of geological discontinuities on rock slopes.
  • Plot poles on an equal area stereonet.
  • Contour pole concentrations to identify maxima indicating failure modes.
  • Failure modes identified by pole concentration patterns:
    • Plane failure (Fig.1a)
    • Wedge failure (Fig.1b)
    • Toppling failure (Fig.1c)

2. Key Failure Mode: Wedge Failure (Clause 3.2.2)

  • Occurs along two intersecting discontinuities.
  • Line of intersection dips towards slope but plunge < slope inclination.
  • More frequent than planar slides.

3. Rock Mass Rating (RMR) Basic Parameters (Table 1)

ParameterRating Range (Example)Rating
Intact Rock Strength> 10 MPa (Point Load)15
Drill Core Quality (ROD)90-100%20
Discontinuity Spacing> 2 m20
Groundwater ConditionCompletely dry15

4. Adjustment Ratings for Rock Slopes (Table 2 & 3)

  • Adjustment factor = F1 × F2 × F3 + F4
  • F1, F2, F3 depend on slope and discontinuity orientation.
  • F4 depends on excavation method.
Method of ExcavationF4 Rating (Adjustment)
Natural Slope+15
Presplitting+10
Smooth Blasting+8
Blasting/Mechanical0
Deficient Blasting-8

5. SMR Calculation Formula:

[ \boxed{ SMR = RMR_{basic} + (F_1 \times F_2 \times F_3) + F_4 } ]


Stereonet Concept (Mermaid Diagram):

graph LR
A[Field Data: Geological Discontinuities] --> B[Plot Poles on Equal Area Stereonet
7Classification of Slope Stability Based on SMR

Slope Mass Rating (SMR) - IS 13365 Part 3

Key Formula:

[ \boxed{ \text{SMR} = \text{RMR}_{basic} + (F_1 \times F_2 \times F_3) + F_4 } ]

  • RMR_basic: Basic Rock Mass Rating from IS 13361 (Part 1).
  • F1, F2, F3: Adjustment factors related to discontinuity orientation, mode of failure, and excavation method.
  • F4: Adjustment for seepage and weathering effects.

Classification of Slope Stability (Table 4):

SMR Value RangeSlope Stability Classification
81 - 100Fully Stable
61 - 80Stable
41 - 60Partially Stable
21 - 40Unstable
< 20Very Unstable

Notes:

  • SMR incorporates joint orientation, fracture spacing, seepage, weathering, and excavation method.
  • Used for preliminary slope stability assessment and landslide hazard zonation.
  • Failure modes considered: Planar slide, wedge slide, toppling failure.

Conceptual flow of SMR calculation:

flowchart TD
    A[RMR_basic] --> B[Calculate F1 (Orientation)]
    A --> C[Calculate F2 (Failure Mode)]
    A --> D[Calculate F3 (Excavation Method)]
    A --> E[Calculate F4 (Seepage & Weathering)]
    B & C & D --> F[Multiply F1 × F2 × F3]
    F & E & A --> G[Calculate SMR]
    G --> H[Classify Slope Stability]

For detailed factor values (F1, F2, F3, F4), refer to IS 13365 Part 3 tables specifying adjustment factors based on joint-slope angle, excavation method, and failure mode.

8Determination of Safe Cut Slope Angle

Determination of Safe Cut Slope Angle (IS 13365 Part 3)

IS 13365 (Part 3) provides a systematic approach to evaluate rock slope stability using the Slope Mass Rating (SMR) method, which helps determine safe slope angles.


Key Formulas:

  1. Slope Mass Rating (SMR):

[ \boxed{ \text{SMR} = \text{RMR}_{basic} + (F_1 \times F_2 \times F_3) + F_4 } ]

  • RMR_basic: Basic Rock Mass Rating (Table 1)
  • F1, F2, F3: Adjustment factors based on discontinuity orientation (Table 2)
  • F4: Adjustment for excavation method (Table 3)

Important Tables:

ParameterRating Range (RMR_basic)Points
Strength of intact rock>250 MPa15
Drill core quality (ROD)90-100%20
Spacing of discontinuities>2 m20
Groundwater conditionCompletely dry15

(Refer Table 1 for full RMR_basic ratings)


FactorVery FavourableFavourableFairUnfavourableVery Unfavourable
F1 (Parallelism)0.150.400.700.851.00
F2 (Dip of discontinuity)0.150.400.700.851.00
F3 (Dip difference)0-6-25-50-60

(See Table 2 for detailed angle ranges)


Excavation MethodF4 Adjustment
Natural slope+15
Presplitting+10
Smooth blasting+8
Blasting or mechanical0
Deficient blasting-8

Stability Classification Based on SMR:

SMR ValueStability
81-100Fully Stable
61-80Stable
9Remedial Measures for Unstable Slopes

Remedial Measures for Unstable Slopes (IS 13365 Part 3)

1. Slope Stability Classification (Clause 3.4 & Table 4)

Slope Mass Rating (SMR) is calculated as:

[ \text{SMR} = \text{RMR}_{basic} + (F_1 \times F_2 \times F_3) + F_4 ]

  • SMR Stability Classes:
    • Fully stable: 81–100
    • Stable: 61–80
    • Partially stable: 41–60
    • Unstable: 21–40
    • Very unstable: <20

2. Remedial Measures (Clause 3.5)

  • Very unstable slopes (<20 SMR): Require re-excavation or major corrective works.
  • Unstable slopes (21–40 SMR): Need extensive corrective measures.
  • Partially stable slopes (41–60 SMR): Use systematic supports such as:
    • Rock bolts
    • Rock anchors
  • Stable to fully stable slopes (>60 SMR): Occasional or no support required.

3. Key Parameters for RMR_basic (Table 1 Summary)

ParameterRating Range (High to Low)Max Rating
Strength of intact rock>10 MPa to <1 MPa15
Drill core quality (ROD)90–100% to <25%20
Spacing of discontinuities>2 m to <60 mm20
Condition of discontinuitiesVery rough to slickensided/gouge30
Groundwater conditionDry to flowing15

4. Typical Supports for Partially Stable Slopes

  • Rock bolts/anchors: Increase slope stability by reinforcing rock mass.
  • Drainage measures: Reduce pore water pressure.
  • Shotcrete or mesh: Surface protection against weathering.

flowchart TD
    A[Assess Slope] --> B[Calculate RMR_basic]
    B --> C[Calculate SMR = RMR_basic + (F1*F
10References to Related Indian Standards

IS 13365 Part 3 (1997) primarily deals with rock mechanics testing procedures and references related Indian Standards for consistency and accuracy.

Key References to Related Indian Standards:

  • IS 2:1960Rules for rounding off numerical values: Specifies how to round off test results or calculated values.
  • Other related IS codes commonly referenced in rock mechanics and testing include:
    • IS 1121 series — Methods of test for soils (for geotechnical context)
    • IS 456:2000 — Plain and reinforced concrete code (for structural context)
    • IS 13827:1993 — Code of practice for rock excavation
    • IS 1893 — Criteria for earthquake resistant design (relevant for rock stability)

Rounding Off Rule (IS 2:1960):

  • Round off to the nearest value based on the digit following the last significant figure.
  • If the digit is ≥5, increase the last retained digit by 1; if <5, leave it unchanged.
Example:
Value = 12.3456, round to 3 decimals → 12.346
Value = 12.3444, round to 3 decimals → 12.344

Summary:

  • Use IS 2:1960 for rounding.
  • Refer to related IS codes for complementary tests and design criteria.
  • Always cite these standards when reporting test results per IS 13365 Part 3.
flowchart LR
    A[IS 13365 Part 3] --> B[Testing Procedures]
    B --> C[Use IS 2:1960 for Rounding]
    B --> D[Refer to IS 1121, IS 456, IS 13827]
    D --> E[Geotechnical & Structural Design]
11Annex A: Technical Committee Composition

IS 13365 Part 3: Annex A - Technical Committee Composition

Annex A lists the detailed composition of the Rock Mechanics Sectional Committee, CED 48, responsible for formulating this standard.


Key Points:

  • Chairman: Prof. Bhawani Singh, University of Roorkee
  • Member Secretary: Shri W. R. Paul, Joint Director (Civil Engg), BIS
  • Members: Experts from diverse organizations including:
    • Irrigation Departments (Roorkee, Haryana, Gujarat, Maharashtra)
    • Central Mining Research Institute (CSIR)
    • Geological Survey of India
    • Central Water and Power Research Station
    • Indian Institutes of Technology (Roorkee, Delhi, Kanpur)
    • National Thermal Power Corporation
    • Central Building Research Institute (CSIR)
    • Various private sector engineering firms and research institutes

Purpose of Annex A:

  • Ensures multidisciplinary expertise in rock mechanics and slope stability.
  • Includes academia, government bodies, research institutes, and industry professionals.
  • Supports development of robust, practical standards for rock engineering.

Summary Table (Excerpt)

RoleRepresentative Organization
ChairmanUniversity of Roorkee
Member SecretaryBureau of Indian Standards (BIS)
MembersCSIR Institutes, IITs, Irrigation Dept., Geological Survey, Power Corporations, Private Firms

This committee composition ensures the standard reflects state-of-the-art knowledge and practical experience in rock mechanics and slope stability.

graph TD
    A[Technical Committee CED 48] --> B(Chairman: Prof Bhawani Singh)
    A --> C(Member Secretary: Shri W. R. Paul)
    A --> D[Members]
    D --> E(Irrigation Departments)
    D --> F(CSIR Institutes)
    D --> G(Indian Institutes of Technology)
    D --> H(Geological Survey of India)
    D --> I(Power Corporations)
    D --> J(Private Engineering Firms)

For detailed member names and affiliations, refer to Annex A in IS 13365 (Part 3):1997.

Popular Questions About IS 13365 Part 3

?How is the Slope Mass Rating (SMR) calculated using this standard?

According to IS 13365 Part 3, the Slope Mass Rating (SMR) is calculated as:

[ \boxed{ \text{SMR} = \text{RMR}_{\text{basic}} + (F_1 \times F_2 \times F_3) + F_4 } ]

Components:

  • RMR_basic: Basic Rock Mass Rating from IS 13365 Part 1.
  • F1, F2, F3: Adjustment factors related to:
    • F1: Orientation of discontinuities relative to slope.
    • F2: Dip of discontinuities.
    • F3: Excavation method or slope geometry.
  • F4: Additional adjustment for seepage or weathering effects.

Stability Classification (Table 4):

SMR RangeStability
81 - 100Fully Stable
61 - 80Stable
41 - 60Partially Stable
21 - 40Unstable
< 20Very Unstable

Summary:

  • SMR refines RMR by considering joint orientation, seepage, fracture spacing, weathering, and excavation.
  • It helps assess rock slope stability for landslide hazard zonation.
Loading diagram...

This method is reliable and straightforward for hilly terrains with exposed rock.

?What are the main failure modes of rock slopes covered in IS 13365 Part 3?

Main Failure Modes of Rock Slopes as per IS 13365 Part 3

  1. Wedge Failure (3D Wedge Slide)

    • Occurs along the intersection of two discontinuity sets.
    • Intersection line dips towards the slope/valley but with plunge less than slope inclination.
    • More frequent than planar slides; planar failure is a special case of wedge failure.
  2. Toppling Failure

    • Occurs along continuous joints dipping against the slope, with strike nearly parallel to slope face.
    • Can be minor (near surface) or deep (large deformation).
    • Failures develop slowly, less prone to sudden rock falls.
  3. Planar Failure (Special case of wedge failure)

    • Sliding along a single discontinuity plane parallel or sub-parallel to the slope face.

Identification Method:

  • Use stereonet plots of geological discontinuities (100-500 readings).
  • Analyze pole concentration maxima to identify failure modes.
Loading diagram...

This approach ensures accurate failure mode determination for safe slope design.

?How do joint orientation and excavation methods affect slope stability ratings?

Effect of Joint Orientation and Excavation Methods on Slope Stability Rating (SMR) as per IS 13365 Part 3

  1. Joint Orientation Adjustment (F1, F2, F3):
    The slope mass rating (SMR) is adjusted based on the orientation of joints with respect to the slope face:

    • F1: Depends on parallelism between slope dip direction (as) and joint dip direction (aj).
    • F2: Depends on the dip of discontinuity (Bj).
    • F3: Depends on the relationship between dip of discontinuity and slope dip (Bi).

    Ratings for F1, F2, F3 vary from 0.15 (very favourable) to 1.00 (very unfavourable) as per Table 2, influencing the stability significantly.

  2. Excavation Method Adjustment (F4):
    Excavation affects slope stability by altering rock mass integrity:

    MethodF4 Rating
    Natural Slope+15
    Pre-splitting+10
    Smooth Blasting+8
    Blasting/Mechanical0
    Deficient Blasting-8
  3. Final SMR Calculation:
    [ \text{SMR} = \text{RMR}_{basic} + (F1 \times F2 \times F3) + F4 ]

  4. Failure Modes Considered:

    • Planar slide
    • Wedge slide
    • Toppling failure

Summary:

  • Favorable joint orientation (high F1, F2, F3 ratings) improves SMR.
  • Better excavation methods (natural, pre-splitting) increase SMR, while poor blasting lowers it.
  • These factors combined guide remedial measures and support design.
Loading diagram...
?What field data and analysis techniques are recommended for determining slope failure modes?

Recommended Field Data and Analysis Techniques for Slope Failure Modes (IS 13365 Part 3):

  • Field Data Collection:

    • Take 100 to 500 readings of geological discontinuities on the rock slope.
    • Measure discontinuity orientations (dip, dip direction, strike).
    • Record fracture spacing, weathering, seepage conditions, and excavation method.
  • Graphical Analysis:

    • Plot discontinuity poles on an equal area stereonet.
    • Contour the pole concentrations to identify maximas (high-density zones).
    • Failure modes are inferred from the pattern of these maximas (e.g., planar, wedge, toppling).
  • Failure Mode Identification:

    • Use patterns of pole concentration maximas as shown in Fig. 1(a), (b), (c) of IS 13365.
    • Cross-reference with SMR (Slope Mass Rating); detailed study is needed if SMR < 60 or slope distress is visible.
    • Consider geological discontinuity sets controlling movement surfaces.

Summary Table of Failure Modes (from IS 11315 Part 1):

Failure ModeGoverning Discontinuity Pattern
Planar SlideSingle discontinuity set dipping out of slope face
Wedge SlideIntersection of two discontinuity sets forming wedge
TopplingDiscontinuities dipping steeply out of slope face
Loading diagram...

This approach ensures reliable identification of rock slope failure modes based on field data and graphical stereonet analysis.

?What remedial measures are suggested for slopes classified as unstable or very unstable?

Remedial Measures for Unstable and Very Unstable Slopes (IS 13365 Part 3)

Based on Clause 3.5 and slope classification by Slope Mass Rating (SMR):

  • Very Unstable Slopes (SMR < 20):

    • Require re-excavation to reshape or reduce slope angle.
    • May need extensive stabilization measures.
  • Unstable Slopes (SMR 21-40):

    • Need extensive corrective measures such as:
      • Rock bolts
      • Rock anchors
      • Drainage improvements to reduce seepage forces
      • Slope regrading or terracing
  • Partially Stable Slopes (SMR 41-60):

    • Supported with systematic supports like rock bolts and anchors.
  • Stable to Fully Stable Slopes (SMR > 60):

    • Require occasional or no support.

Important Note:

  • A detailed study is necessary if SMR < 60 or if the slope shows distress signs.
  • SMR considers joint orientation, seepage, fracture spacing, weathering, excavation method, and failure mode (planar, wedge, toppling).

SMR Formula (Clause 3.4):

[ \text{SMR} = RMR_{basic} + (F_1 \times F_2 \times F_3) + F_4 ]

Where factors (F_1) to (F_4) adjust for slope-specific conditions.


Loading diagram...

This ensures slope safety by matching remedial actions to stability levels.

Need Detailed Clause Answers?

Ask AI about any clause, requirement, or provision in IS 13365 Part 3. Get instant, clause-cited responses powered by our indexed library.

Free tier includes 150 queries (50 AI + 100 Reference) · No credit card required