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Liman irrigation system

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and the destruction of infrastructure. Also, the infiltration is insufficient because of the water's velocity, even though the runoff would be able to allow for the growth of trees in appropriate places. The aim of building limans is to stop flash floods and to increase water infiltration, thus
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Ffolliott, P.F. et al. 2000. International Arid Lands Consortium: Better Land Stewardship in Water and Watershed Management. USDA Forest Service Proceedings – Rocky Mountains Research Centre P-13: p.335–338.
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Angel, R., & Conrad, R. 2009. In situ measurement of methane fluxes and analysis of transcribed particulate methane monooxygenase in desert soils. Environmental Microbiology 11(10): p.2598–2610.
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Brunori, A., Nair, P.K.R., & Rockwood, D.L. 1995. Performance of two Eucalyptus species at different slope positions and aspects in a contour-ridge planting system in the Negev Desert of Israel.
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in arid areas. In Proceedings, International Conference on Water Resources Management in Arid Regions. 23–27 March 2002, 107–122. Kuwait: Kuwait Institute for Scientific Research Available at:
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Because desert crusts prevent rainwater from infiltrating the ground, they generate surface run-off that can lead to flash floods and to top-soil erosion. Limans prevent both the loss of
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Limans are structures with small dams which catch runoff from a wadi to hold about 400-600mm of water, which suffices for the growth of drought-hardy tree species. Limans can be built
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is slowed by the dam, thus flooding a small area and allowing the water to infiltrate into the soil. This way, a small groves of trees can be sustained in the desert. The
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Bruins, H.J.; Evenari, M.; Nessler, U. (1986). "Rainwater-harvesting agriculture for food production in arid zones: the challenge of the African famine".
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height should be 3–4 times the designed water depth, and the outlet should be to the side of the main flow to prevent direct through flow. Also,
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Before the invention of Limans, their creators as well as scientists expected several positive and/or negative impacts:
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They expected a negative soil salinisation due to salt deposition and/or high evaporation rates. This was not the case.
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No literature could be found as of June 2012, which suggests that the issue might not have been studied yet.
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uptake, but it could not be measured in limans. Instead, they found a shallow zone of methane production.
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is the name for an artificial earthen construction used to collect floodwater by damming a desert
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was mostly used in the past. However, some scientific studies have had better results with
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resources, which are becoming increasingly rare in arid ecosystems. Remaining
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http://onlinelibrary.wiley.com/doi/10.1111/j.1462-2920.2009.01984.x/abstract
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wherever tributary wadis widen or come onto a large plain with potential
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regulates the level of the water to prevent the destruction of the
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http://www.fs.fed.us/rm/pubs/rmrs_p013/rmrs_p013_335_338.pdf
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Prinz, D. 2002. The role of water harvesting in alleviating
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So far, no ecological research has been conducted on
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Index

Liman (landform)

JNF
Negev Desert
Israel
wadi
runoff water
JNF-KKL
Negev Desert
desertification
groundwater
soil humidity
wadis
rains
wadis
flash floods
soil erosion
growth
drought-hardy
tree
species
vegetation
arable land
check-dam
runoff waters
spillway
check-dam
embankment
grazers
soil compaction

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