Liman irrigation system

Source: Wikipedia, the free encyclopedia.
Not to be confused with Liman (landform).
Negev Desert
.

A Liman (from Greek λιμήν) in

Negev Desert.[1]

Introduction

Limans were built in order to fight

flash floods. The result is massive soil erosion 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.[3] The aim of building limans is to stop flash floods and to increase water infiltration, thus sustaining the growth of drought-hardy tree species and vegetation
underneath them.

Design

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.[3] Limans can be built wherever tributary wadis [...] widen or come onto a large plain with potential arable land [...]. A check-dam [...] is built to retain runoff waters [...]. A spillway regulates the level of the water [...] to prevent the destruction of the check-dam..[4] The embankment 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, grazers should be excluded from the site to prevent soil compaction which would in turn decrease water infiltration.[3]

Suitable tree species

Because of its fast growth, Eucalyptus occidentalis was mostly used in the past.[3] However, some scientific studies have had better results with Eucalyptus sargentii.[5] Overall, any drought-hardy species are suitable, such as tamarind, acacia, prosopis, pistachio, eucalyptus, date palm and carob[citation needed].

Effects

Before the invention of Limans, their creators as well as scientists expected several positive and/or negative impacts:

  • They expected a negative soil salinisation due to salt deposition and/or high evaporation rates. This was not the case.[6]
  • Carbon sequestration: Because of the biomass increase, a CO2 uptake is expected.[7]
  • Scientists were hoping for a methane uptake, but it could not be measured in limans. Instead, they found a shallow zone of methane production.[8]
  • 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 surface runoff and of topsoil, as well as plant nutrients. On top of that, they provide a controlled place to deposit these resources.[1]
  • So far, no ecological research has been conducted on biodiversity within limans.[1]

See also

References

  1. ^ a b c "Limans". www.kkl-jnf.org.
  2. ^ Prinz, D. 2002. The role of water harvesting in alleviating water scarcity 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: "Archived copy" (PDF). Archived from the original (PDF) on 2012-03-24. Retrieved 2012-06-21.{{cite web}}: CS1 maint: archived copy as title (link)
  3. ^ a b c d Wilson, G (1980). "Limanim" (PDF). Landscape Australia. 80 (3): 159–163.
  4. doi:10.1016/0143-6228(86)90026-3
    .
  5. ^ 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. Forest Ecology and Management (75): p.41–48. PDF
  6. ^ 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. http://www.fs.fed.us/rm/pubs/rmrs_p013/rmrs_p013_335_338.pdf
  7. ^ No literature could be found as of June 2012, which suggests that the issue might not have been studied yet.
  8. ^ 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. http://onlinelibrary.wiley.com/doi/10.1111/j.1462-2920.2009.01984.x/abstract
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