Chapter 1 Hydrological Cycle
Page 1: Introduction to Hydrology
Title: Surface and Groundwater Hydrology (CE30052)
Page 2: Understanding Hydrology
Definition: Hydrology is the study of water in the environment.
Hydrologic Cycle: Refers to the continuous circulation of earth’s water resources in solid, liquid, and vapor phases.
Links the atmosphere, land, and oceans.
Powered by solar energy.
Page 3: Components of the Hydrologic Cycle
Key Processes:
Precipitation: Water falls to the earth in various forms (rain, snow).
Evaporation: Water vaporizes from oceans and land surfaces.
Infiltration: Water enters the ground, replenishing groundwater.
Runoff: Water flows over land surfaces into streams and rivers.
Transpiration: Water released from plants into the atmosphere.
Visual Representation (Fig. 1.1): Highlights the interconnections among precipitation, evaporation, infiltration, and runoff.
Page 4: Water Table and Flow Dynamics
Groundwater Hydrodynamics:
Water Table: The upper surface of groundwater.
Groundwater Flow: Movement of water underground.
Discharge and Recharge: How groundwater is replenished and discharged.
Statistics on Water Movement:
Groundwater Discharge: 38
Surface Discharge: 61
Evaporation from land: 39
Precipitation on ocean: 424
Page 5: Components of Hydrological Cycle
Transportation Components:
Precipitation, Evaporation, Transpiration, Infiltration, Runoff.
Storage Components:
Surface storage (e.g., ponds, lakes, reservoirs).
Soil moisture storage.
Groundwater storage.
Page 6: Hydrologic Cycle Transportation Components
Visual representation (Fig. 1.2): Shows how various components interact within the hydrologic cycle:
Evapotranspiration, Stream Flow, Infiltration, Base Flow, Groundwater Flow.
Page 7: River Catchment Illustration
Schematic Representation (Fig. 1.3): Describes the catchment of River A, highlighting key features such as:
Watershed/Dive: The shared area where water flows into a river.
Tributary Relationships: Streams flowing into River A.
Page 8: Water Budget Equation
Water Budget Principle:
Equation: Mass inflow – Mass outflow = Change in mass storage.
Example: P (Precipitation) - R (Runoff) - G (Groundwater) - E (Evaporation) - T (Transpiration) = ∆S (Change in Storage).
Detailed Breakdown:
S = Total storage, including seasonal variations (Ss + Ssm + Sg).
Pages 9-10: Hydrology Problems
Example Problem (Lake Water Budget):
Calculation of water elevation change based on inflow and outflow statistics.
Second Problem (Catchment Rainfall):
Calculate the amount of water unavailable for runoff due to infiltrations such as transpiration and evaporation.
Discusses runoff coefficients and effects of afforestation on runoff.
Page 11: Reservoir Withdrawal Rate Estimation
Withdrawal Calculation:
Estimation of constant withdrawal rate from a reservoir considering inflow, evaporation, and seepage losses.
Important for managing water resources in the engineering field.
Page 12: World Water Balance
Breakdown of Water Resources:
Data on various water bodies: oceans, groundwater, ice caps, lakes, rivers, wetlands, etc.
Provides a percentage distribution of total water vs. freshwater.
Key Statistics:
Oceans hold 96.5% of total water.
Freshwater sources are very minimal compared to saline water, with ice caps and glaciers comprising a significant volume.
Page 13: Applications in Engineering
Engineering Applications of Hydrology:
Irrigation: Ensuring agricultural water supply.
Water Supply: Managing and distributing water resources.
Flood Control: Mitigating flood risks through planning and structural interventions.
Water Power: Utilizing hydrological resources for energy.
Navigation: Maintaining waterway conditions for transportation.