1.
2
2 a
2b
2c
Diagram
aexe feetag to Tacre feething to myl. - million gallons for day = 0.32585 cubic feet / second to cubic meter per second liftels to m3/s. = 0.0282/68 4 6 592 0 inches/hour ainfall to mm/day rainfall I inch/ hour ainfall to mm/day rainfall - 2.5 1 inch = 25 4* num. (1) short tons acre-day to my hectare year.. I short fons per arre day to ing per hectare your 0.00643 7 57753 ( inches/ of to cm/oc. tinches / degree fahrenheit - 1.8 cml degree celsius.
The 2. The recycling of water through continuous movements in air on earth's surface and under the ground Catmosphere in whole) is known as hydrological cycle or water cycle. The important components (preuss) involved in hydrological cycle arel vaporisation, precipitations, infiltration, percolation, Surface run off, condensation, evaporation, and transpiration or evapotranspiration. Infiltration and Percolation..
v piguar (a) It Infiltration and Percolation. Infiltration is the brouss of entering of water into the Soil through ground Surface. It goes vestically and happens at uppermost straturn of soil. It is measured in mm/hr on in/hr , it is fast in beginning Stage - and slow at later stage.. whereas Pescolation is the breess of passing of ligeid through a filter. It happens at far de foth under the ground and accompanied with vertical movement, joining of water table. It is slower in speed as compared to infiltration.
6 Base flow is subsurface flow occuring at shallow depth above ground water table. It is delayed fordeess of lateral flow. C Constant) Whereas Interflow is actual lateral movement of water which occurs during precipitation and happens through upper soil surface. It happens in unsatured or vadose zone. O traforation is surface level procedure which oneers'
oll surface. vadose zone. It happens on unsatured on whereas and! o traposation is surface level Procedure which wers in warm or cold condition and may happen from living or non living surface. Troms pisation is physiological process which ours in foresence of sunlight and happens only from living bodies. It has remarkable importance in blant wofe. Evaketoonisfization is a preuss through which is 6 Comboration of evaporation and fronspirate on It is responsible for I 715% of atmosphere water vakor. In real, evapotronspiration is combined form of - erakoration of water from soll/earth's surface and tonskisation of moisture from Plants surface which results in freispitation.
I precipitation ↑ Evapotsons pirates on 7 Surface runoff Initial losses Impornas Penas Root zone Interflow Infiltation onsomitionron Percolation saturated zone Ground fwater flow- Recharge