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Desertification Indicator System for Mediterranean Europe


1. Definition

Name

RUNOFF WATER STORAGE

Brief definition

Volume of runoff water stored in soil or in small ponds.

Small pond around an olive tree concentrating water runoff and increasing infiltration and starage of water into the soil (photo by C. Kosmas)

Unit of measure

mm, or % of the total runoff water stored.

2. Position within the logical framework DPSIR

Type of Indicator

Response

3. Target and political pertinence

Objective

To increase soil water storage and water availability to the growing plants.

Importance with respect to desertification

Whenever water flows over unprotected soil it may pick up and carry along soil particles. If such flows are concentrated by natural topography or works of man rills or gullies may develop and destroy valuable farm land by transporting large amounts of soil sediments.

International Conventions and agreements

Transboundary and interbasin legal agreements.

Secondary objectives of the indicator

Percentage of water demand satisfied, economic and environmental issues.

4. Methodological description and basic definitions

Definitions and basic concepts

Storage of water runoff is defined in terms of land management for reducing surface water runoff and increasing soil infiltration rates. For example, presence of adequate shrubby or annual vegetation cover, construction of terraces, shallow ploughing of the soil parallel to the contour lines, concentrating the runoff water in small ponds and retarding runoff, keeping plant residues on the soil surface, etc. Contouring, strip cropping, and land terracing are important conservation practices for controlling water erosion. These management practices require the adjustment of the tillage and crop-row direction from uphill and downhill to a contour operation. Small ridges and depressions increase the storage of water on the surface, thus increasing infiltration and storage of water in the soil profile. Terraces are a method of erosion control accomplished by constructing broad channels or benches across the slope or building walls using stones.

Benchmarks Indication of the values/ranges of value

  • adequate,
  • moderate,
  • low,
  • very low,
  • no measures for runoff water storage

Methods of measurement

Assessment in the field if management practices for runoff water storage are applied, and how efficient they are.

Limits of the indicator

Measurement of the indicator is based on self-assessment subject to personal judgement.

Linkages with other indicators

Rainfall, Vegetation cover, Slope gradient, Tillage operations

5. Evaluation of data needs and availability

Data required to calculate the indicator

Detailed management practices data applied to each farm.

Data sources

Necessary data are usually available and accessible and the cost/benefit ratio may be reasonable.

Availability of data from national and international sources

Data may be obtained from various regional institutions involved in the collection and analysis of land management practices.

6. Institutions that have participated in developing the indicator

Main institutions responsible

Agricultural University of Athens, Greece

Other contributing organizations

Universities of Lisbon, Murcia, Basilicata, Amsterdam, Leeds

7. Additional information

Bibliography

Troeh, F., Hobbs, J., and Donahue, R., 1980. Soil and water conservation for productivity and environmental protection. Prentice-Hall, Inc.Englewood Cliffs, N.J., 718 p.

Other references

Follett, R., and Stewart B., 1985. Soil erosion and crop producr\tivity. American Society of Agronomy. Madison Winscosin. USA

Contacts Name and address

Dr Constantinos Kosmas
Agricultural University of Athens,
Laboratory of Soils and Agricultural Chemistry,
Iera Odos 75,
Athens 11855, Greece
email: lsos2kok@aua.gr