2006
DOI: 10.1080/10641260500341320
|View full text |Cite
|
Sign up to set email alerts
|

Surface Water–Groundwater Interactions Between Irrigation Ditches, Alluvial Aquifers, and Streams

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

2
41
0

Year Published

2012
2012
2024
2024

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 64 publications
(43 citation statements)
references
References 36 publications
2
41
0
Order By: Relevance
“…Much recent work has focused on acequia hydrology, including surface water-groundwater interactions [13], deep percolation and shallow groundwater levels [14], water movement through the vadose zone during irrigation [14], and effects of hydrology on riparian habitat and agroecosystem functions [4]. Other approaches have focused on acequia preparedness for climate change or community restructuring [2], or the economics related to acequia participation, alternative water sources, and land fragmentation impacts on acequia resilience (i.e., the ability of the system to quickly respond to disruptive events) [4].…”
Section: Populationmentioning
confidence: 99%
“…Much recent work has focused on acequia hydrology, including surface water-groundwater interactions [13], deep percolation and shallow groundwater levels [14], water movement through the vadose zone during irrigation [14], and effects of hydrology on riparian habitat and agroecosystem functions [4]. Other approaches have focused on acequia preparedness for climate change or community restructuring [2], or the economics related to acequia participation, alternative water sources, and land fragmentation impacts on acequia resilience (i.e., the ability of the system to quickly respond to disruptive events) [4].…”
Section: Populationmentioning
confidence: 99%
“…For example, studies indicate that typical canal losses range from 16% to 43% of channel flow [13][14][15], and percolation rates below crop rooting zones as a percentage of irrigation water applied range from less than 23% to 60% or more [16][17][18][19]. Unlike evapotranspiration losses that take water out of the system and preclude future use, canal seepage and field percolation perform the important function of recharging groundwater as demonstrated with hydrodynamic, chemical, stable isotope, and simulation modeling approaches [19][20][21][22][23][24][25]. This water that recharges the shallow aquifer can then become groundwater flow that returns through the subsurface to connected streams [15].…”
Section: Hydrologic Connections Between Acequia Irrigation Systems Amentioning
confidence: 99%
“…Here these losses were found to provide a significant amount of recharge to the shallow groundwater system; this water returns to the river maintaining stream baseflows after peak runoff (Fernald and Guldan 2006, Fernald et al 2007. Within the study area groundwatersurface water dynamics in the irrigated agriculture driven by decreased surface water infiltration and increased groundwater pumping during period of limited surface supply can be addressed indirectly.…”
Section: Surface Water-groundwater Connectionsmentioning
confidence: 99%