Check your knowledge… To get warmed up, please answer three questions to check your understanding. If you are not familiar with some of the terms used, don’t worry! We will define these terms in the module.
|Water Sources||Amounts of Water|
|Discharge to Surface Water||40 units|
|Deep Drainage||10 units|
|Surface Water Seepage||30 units|
As you examine issues impacting you Natural Resource District, one important aspect of water resource management is maintaining adequate groundwater levels. The map below shows groundwater level changes in Nebraska
To make informed decisions about this issue, it is important to understand how water moves into and out of a groundwater system.
Let's begin by exploring groundwater levels in a Nebraska location.
Now that you know what is happening to groundwater levels in this location, you can begin to think why levels are declining
To understand this change, it is helpful to thing of groundwater as a system. While system interactions are complex, three basic components determine groundwater levels in your area. The video below explains these three components.
Under natural conditions, the average amount of water recharged into the system is equal to the amount of water discharged. The volume of water in storage generally does not change and the groundwater system is in balance.
However, if the system has unequal amounts of recharge and discharge, the system is out of balance and a change in groundwater levels will result.
Drag and drop the gray boxes to the correct location to indicate how water in storage is affected by various amounts of inputs and outputs.
When a system has more inputs than outputs, water storage will increase. When a system has more outputs than inputs, water storage will increase.
Rivers, lakes, streams, and irrigation canals are all examples of surface water bodies. In some areas, surface water can “leak” down through sediments to recharge the groundwater system.
Sometimes plants are unable to utilize all irrigation water that is applied. Some excess irrigation water may run into surface waters, while some excess water may drain below crop roots (“deep drainage”) and eventually recharge groundwater.
Most groundwater recharge comes from precipitation. Some precipitation will run off the land surface and into surface water bodies. Other precipitation that is not utilized by plants or evaporated will infiltrate below the plant roots and may eventually recharge groundwater.