‘In-field, agricultural, soil based interventions’

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Countryside and Community Research Institute

Presentation by Ben Thorne (FWAG) at the Rural SuDS Natural Flood Management Conference Agenda, Wednesday 25th January 2017

Environment

Natural Flood Management
in Practice
Ben Thorne, FWAG SW

AfterBefore
Bunded Scrape
Intercepting flow pathway in valley
After
Bunded scrape to
intercept flow pathway

Construct ditch to take
run-off from road to
pond
Construct
footbridge over
ditch
Construct ditch/swale
to channel water into
pond
Bund constructed from site soil
Area to be excavated to create
pond Use soil arisings to form
bund
Not to scale
Indicative view only

Ground water recharge is the process whereby the amount of water present in or flowing through the interstices of the sub-soil increases by natural or artificial means. Rainfall is the principal source for replenishment of recharge of ground water. Other sources include recharge from rivers, streams, irrigation water etc. An unconfined aquifer is recharged directly by local rainfall, rivers, and lakes, and the rate of recharge will be influenced by the permeability of overlying rocks and soils. A confined aquifer, on the other hand, is characterized by an overlying bed that is impermeable, and local rainfall does not influence the aquifer. It is normally recharged from lakes, rivers, and rainfall that may occur at distances ranging from a few kilometers to thousands of kilometers.

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