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2.2 Legend

The consolidated erosion map legend has been kept open and flexible enough to be adequate and adaptable to a reasonable variety of specific Mediterranean geographical backgrounds which are all related to coastal zone environments, but with numerous local micro-climatic, lithologic and land use variables. Special emphasis has been given to the following aspects:

• agro-ecological or big-geographical zoning for different mapping scales and surveying conditions;

• soil surface state assessment (surface crusting and sealing) and the consequences on run-off and infiltration water dynamics);

• mechanical and/or chemical changes occurred in soils as a result of specific cropping or land use techniques (compacting)1;

• specific identification and assessment of erosion-affected areas due to infrastructure

1 Features to be considered as part of the lithology/parent material parameters to be integrated in the phase of erosion status mapping depletion (roads, old terraces, check dams, etc.).

Overall geographical environments can be subdivided in two broad categories:

Stable, non-erosion-affected areas, and
Unstable, erosion-affected areas.

The erosion map legend as described in Box 1 has been prepared according to the referred landscape classification as a basic reference framework and a guide to both a predictive and descriptive diagnosis.

BOX 1: Legend

A. PREDICTIVE MAPPING: INFERRED GLOBAL EROSION HAZARDS

Symbols

(0)

none (Equivalent to stable non-used wasteland in descriptive mapping: 010)

(1)

very slight

(2)

slight

(3)

moderate

(4)

severe

(5)

very severe

B. SITE-DESCRIPTIVE MAPPING: GRADE OF STABILITY/EROSION PROCESSES1

I. Stable, non-erosion-affected areas (*)

00

stable, non-used wasteland (rock outcrops, cliffs, stony or sandy areas)

01

stable, unmanaged areas with potential for forestry use only

02

stable, unmanaged areas with agricultural potential (crops and pasture)

03

stable, managed areas with forestry use only

04

stable, managed areas with agricultural use (crops and pasture)

Rehabilitated areas by means of:

05

natural or artificial re-vegetation

06

physical infrastructures (terraces, check dams, etc.)


*Grade of instability risk


Assessment of instability risk for all stable environments (00 to 04) and of risk for rehabilitated environments, i.e. 05+06 (i.e. a risk in the first years of rehabilitation;) to be expressed by a complementary digit (0 to 3) to the original stable unite' code:


0: No risk (= highest grade of stability)


1: Low to moderate


2: High


3: Areas in hazardous/precarious/critical state (Stability threshold = highest grade of instability risk)


Example :

03 = stable managed areas';
032 = stable managed areas with a high erosion risk



*Identification of main causative agents


Instability risk assessment may be reinforced by the identification of its most probable/prevailing causative agents inherent in the landscapes' main basic components, i.e.:


t: Topography


g: Geology


v: Vegetation


h: Human activities


a: Animal activities (trampling, terracing, etc.)


Extra codes might be freely added according to local specific contexts and situations.


Example: 023 g = stable managed areas with erosion risk mainly due to geologic factors.

II. Unstable areas (**)

Splash erosion

A1

localized (<30% of the area is affected)

A2

dominant (30-60%)

A3

generalized (>60%)

Sheet erosion

L1

localized

L2

dominant

L3

generalized with soil profile removal

Lx

= unreclaimable areas due to total soil removal

Rill erosion

D1

localized

D2

dominant

D3

generalized

Gully erosion

C1

individual gullies

C2

localized gully networks

C3

dominant

C4

generalized

Cx

= unreclaimable areas due to generalized band lands

Wind erosion

E1

localized loss of topsoil/overblowing/deflection

E2

dominant

E3

generalized

Ex

= unreclaimable areas due to total sand or sediment burying or topsoil removal

Mass earth movements

M1

local gravitational soil creep/solifluction

M2

localized land slides/mudflows

M3

dominant

M4

generalized

MX

= unreclaimable areas due to total slope slides

Symbols

Water or sediment excess

W1

areas periodically flooded and/or sediment buried

W2

areas permanently flooded and/or sediment buried/waterlogged areas

Degradation induced by land management

S1

soil compacting

K1

soil crusting

Z1

cattle trampling/terraceting

H1

salinisation

Associated processes


See "Note" in pare (**)


Multiple processes


P1 P2 P3 etc. (for description of different closely interacting erosion processes)


**Erosion expansion trend (rate)


Assessment of erosion rate/trend for all unstable erosion-affected areas to be expressed by a complementary digit (0 to 3) to the original unstable units' code:


0: Trend to stabilization, recession or limitation of spatial expansion


1: Trend to local expansion or intensification


2: Trend to widespread expansion or intensification


3: Trend to increase generalized degradation towards an irreversible state


Example:


L2 = dominant sheet erosion


L23 = dominant sheet erosion with a trend towards generalization and an irreversible state (Lx type units)


Note: All multiple or mixed but clearly identifiable erosion processes can be mapped by associating or combining the corresponding codes (the sequence of the codes should be established according to the relative importance of the processes: first code = the most important process):


Example: L11/C12 = Localized sheet erosion combined with dominant gully networks with a trend to widespread expansion or intensification.


Point/line erosion data (Individual erosion processes)

1 Refer to the glossary for the definition of terms

3. Procedures


3.1 General methodological scheme
3.2 First phase: Predictive approach
3.3 Second phase: Descriptive approach
3.4 Third phase: Integration


3.1 General methodological scheme

As already referred to in the general description of the methodology (Ch.2.1), the basic procedure scheme consists of 3 clearly defined phases:

Predictive phase which leads to the mapping of erosion status homogeneous units providing the basic cartographic canvas as far as general erosion potential and trends are concerned;

Descriptive phase which identifies and assesses actual on-site erosion processes as well as the different grades of erosion proneness and evolution trends;

Integration phase the main output of which is the final consolidated rainfall-induced erosion map as a result of overlapping and integrating predictive and descriptive qualitative data.

The predictive phase mainly consists of desk and office data processing by means of 7 different steps:

• Steps 1 and 2: Preparation of slope classes and lithofacies maps;
• Step 3: Erodibility map by overlaying slopes and lithofacies;
• Steps 4 and 5: Preparation of land-use and vegetation cover maps;
• Step 6: Soil protection map by overlaying land use and vegetation cover maps;
• Step 7: Erosion status map by overlapping erodibility and soil protection maps.

The descriptive phase is basically performed in the field by direct observation and control, using the predictive erosion status map as both a cartographic and thematic reference canvas. Field observation should be supported by photo-interpretation, particularly during the preliminary steps which consist of the identification of the stability grade, dominant erosion processes and evolution trends within the various erosion status units.

The integration phase produces the final consolidated erosion map by consolidating all predictive and descriptive data.

The comprehensive graph shown in Fig. I-2 summarizes the overall methodological sequence and clearly identifies the various mapping phases including the final integration leading to the consolidated erosion map.

For all overlaying and integration procedures envisaged, the use of GIS as an efficient tool, highly appropriate for the decision-making process, is recommended.

It is emphasized that the purpose of the map and its future target users have to be clearly defined before starting with the mapping exercise. Erosion mapping cannot be understood as an end itself, but must always aim for indicating needs for and possibilities of future soil conservation activities by the means of planning both short term curative programs and longer term preventive policies. The respective planning steps will include the identification of extreme situations as well as future priorities of action and the respective curative / preventive measures.


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