Soil degradation
Soil has been given a place of mother in many cultures of the world. As a mother plays an important role in taking care of her child, a similar role is played by soil[H1] . Soil provides greater support to big buildings, houses, industries. It also acts as a layer for road construction, which is one of the mean for transportation. It is therefore[H2] very hard to imagine about food production without quality soil. Accordingly to the Natural resources conservation service USA soil is defined as – “The unconsolidated mineral or organic material on the immediate surface of the Earth that serves as a natural medium for the growth of land plants”. For the last few centuries, the world population has been rapidly increasing. Consequently, the demand for food is also gradually increasing. Soil has been affected by number of reasons including urbanization, natural processes, human activities, and many more. Degradation of the soil is its displacement from one place to another. This kind of movement is forced by natural calamities, improper cropping as well as ad hoc land management practices.. There are different natural calamities such as high velocity wind, high intensity rain, topography and where[H3] are also human activities such as intensive use of fertilizer, over irrigation, cutting vegetation, non adoption of soil conservation methods, overgrazing and shifting cultivation become responsible for such kind of movement of soil causing degradation.
Soil Degradation
“Soil degradation is on the increase worldwide, especially in the countries within the tropics. Mismanagement of arable areas by farmers and grazing areas by livestock owners is one of the major causes of soil degradation” (FAO 1999[H4] ). Sustainable management system is needed to be introduced in such areas to manage the loss of soil effectively.
( Images source- Google)
Table no. 1
Estimated Excessive World Soil Erosion Loss
Country
|
Total cropland
(million ha)
|
Excessive soil loss
(million mg)
|
United states
|
167
|
1,524
|
Soviet Union
|
251
|
2,268
|
India
|
140
|
4,716
|
China
|
99
| |
Other
|
607
|
11,201
|
Total
|
1265
|
23,337
|
(Table taken from Textbook, The nature and properties of soil, by Nyle C. Brady p-433, Source- Brown and wolf (1984))
There are different reasons of soil degradation which are presented and explained as follows.
Soil Leaching
As per[H6] the dictionary meaning of leaching, it is the process of removal of soluble constituents because of the action of the force of percolating liquid (thefreedictionary.com). The high amount of rainfall, temperature are having direct proportionality with loss of top soil material. These materials often are valuable elements. The displacement of top material results into the compact and dry surface of top soil. Water pollution is an another issue caused by leaching process, as the fertilizers are leached from drain soil and contaminate water in ponds, lakes and rivers. In tropics because of deforestation the soil is losing its fertility. Even though the leaching of nutrients form soil occurs naturally, for example because of high rainfall and temperature, human activities like deforestation, excessive use of fertilizers, improper land management, irrigation management, improper cultural operations are also became causes of the same. Natural soil erosion occurs due to high wind velocity, water and human activities as already mentioned. It is very much important to understand the causes of erosion before considering its management.
Steep lands
Accordingly to the Land and plant nutrients management system, FAO “ in the context of agricultural problem soils, Steepland are areas where a high slope inclination dominates the problems related to agricultural land use”. The soils of Steepland are generally found shallow[H7] because of the active erosion and slope % is ≥ 12[H8] . As per[H9] the classification of world reference base, the soils of Steepland can be categorized in to the following soil groups: Andosols, Arenosols, Calcisols, Leptosols, Regosols and Cambisols.
Surface, Channel, and mass erosion are the different types of steepland erosion. The relative interactions between climate, soil topography and vegetation determine the extent of steepland erosion and any changes of these compositions may result in the variation of steepland erosion.
Surface erosion
Sheet erosion and rill erosion are two kinds of surface erosion where top soil materials are removed by the raindrop, rain film and then they saturate in the form of sheet and rill. We may find that surface erosion is minimal in undisturbed forest because of infiltration rates exceeds rainfall. Lack of permanent channel is the characteristic of surface erosion. Out of other known methods of predicting surface erosion, the famous one is that universal soil loss equation which is developed by department of agriculture, United States for agricultural lands. Attempt to apply it to steepland forest area s[H10] generally have been unsuccessful- mainly because of the invalid basis assumption that most erosion from forest soils results from sheet overland flow (Robert and Ziember1986,p-9[H11] ). Many attempts including contour terracing and mulching, grass seeding are being developed to control the surface erosion. To reduce the impact of raindrop and energy of surface sheet to establish the network of roots to hold the top soil materials (Soil particles), As it is compared to other kinds of erosion, surface erosion has been given least importance.
A= RKLSP
Where,
R= Climatic erosivity,
K= Soil erodibility
L= slope length
S= slope gradient or steepness
C= cover and management
P= erosion control practice.
Channel erosion
Displacement of material from gully or channel is nothing but [H14] the Channel erosion. This displacement would be of any single particle or whole sediment derived. The size of material being moved in transportation is directly vitiated with the extent or amount of channel. Channel erosion can be effectively managed by keeping the erodible materials in existing channel, by placing large organic debris into small perennial channels, by improving micro drainage network, increasing surface runoff from bare and compacted soils.[H15] On steepland, the formation of gully is considered as a crucial process where the slope angle is critical and soil properties and surface runoff have a direct impact with the slope angle. Extent of runoff, footpath and soil drill have a positive impact on gully/ channel erosion.
Mass erosion
Mass erosion relates to the movement of enormous [H16] of soil or rock. In steep lands mass erosion includes a large variety of process that range from slow and subtle deformation of the soil mantel[H17] to rapid, discrete failure of hillside and stream channels(Robert R. Ziemer[H18] 1886, p-11). It is critically responsible for the movement of the soil particles from hill slopes to stream channels in undistributed forests. Land management activities of course![H19] dramatically increases the probability of mass erosion.
“Creep” is the most common and downslope movement of mantel in steep lands but unfortunately less documented. It occurs in cohesive soils at varying rates and depth.
As stated earlier[H20] it is important to understand ‘how’ and ‘where’ land management programme should be operated. In addition to this, proper planning is also an another requirement to achieve the desired results. Well planned work on the selected site will decide the success on eleventh hour. Technical knowledge in turn has a significant role to play in all of these respects before implementing the erosion management programme.
In most part of the world like in Asia, China, America, Africa, steep lands are economically helpful to grow the crops and contribute in food production, but the soil erosion and surface runoff are the real constraints to exploit the natural advantages of the steep land. According to Purnell (1986), 45% of the hillside are being cultivated in Nepal, and in Ethopia, 54% land area is having slope exceeding 8%, (Source R.lal,p-338 1990)
% of land area by slope class
| |||||||
Slope %
|
Africa
|
Southwest Asia
|
South America
|
Central America
|
Southeast Asia
|
Total area 106 ha
|
%
|
0-8
|
58
|
45
|
52
|
35
|
40
|
3340
|
51
|
8-30
|
34
|
31
|
30
|
40
|
31
|
2107
|
33
|
More than 30
|
8
|
24
|
18
|
25
|
29
|
1048
|
16
|
(Source- R. Lal, 1990 p-339)
Principles of Erosion control.
Major principle of the erosion control is to avoid the loss of soil during heavy rainfall by covering it with protective layers. Different agricultural practices including sod culture and mulching with the help of plastics helps to prevent the soil loss. In contrary to this, the disposal of excess of water and sediment deposition comes under engineering techniques. “The strategy for minimizing soil erosion risks on steeplands, lies in erosion prevention or management”(R.Lal[H22] , 1990 p-341). Under erosion prevention method, surface runoff is reduced while improving the structure of soil where as under Erosion management, the importance is given to decrease the runoff velocity with the transport of sediment with[H23] special devices. Crop and soil surface management are the key elements of erosion prevention methods where the agroforestry, cropping systems and crop husbandry comes under the crop management and tillage, residue management and soil structure improvement comes under the surface erosion management.
On the other hand, safe water disposal and surplus storage of water are the key elements of erosion management. Disposal of water is done through terraces, drop structure, and gabiens, and reservoirs, tanks and dams are used to store the water[H24] .
Agrobioforestry: Active role in Steepland management.
Agroforestry is the kind of agricultural system where agricultural crops are grown with other trees and animal rearing on fixed unit of land. Agroforestry plays an important role in maintaining the ecological efficiency with proper and adequate cycle of nutrient flow. Agroforestry is the best option to utilize the Steepland where fruit trees like Mango, ber,
Citrus can be grown economically with the trees Acacia catechu, Dalbergia sissoo, Anacardium occidentale (Cashew), Bombax ceiba, Santalum album, Acacia nilotica, Schima wallichii, Michelia doltsopa, Pterocarpus dalbergioides,Albizia lebbek,etc. The main aim behind adopting the Agroforestry is to maintain and sustain the yield with effective erosion control.
“Agroforestry systems have also been successfully used in restoring eroded lands in Rwanda. At Nyabisindu, a complex system combining trees, animals and crops was developed (Dover and Talbot, 1987; Laizer et al.,1987)”. [H25] the above mentioned plantation of trees, help to establish the erosion control strip and overall plantation contribute in higher yield.
Agroforestry has been becoming a useful technique or practice in reducing the soil erosion. “Usefulness of Agroforestry systems in erosion control and in stabilizing steeplands has demonstrated in Java(Wiersum,1981;1984) Phillippines (Pacardo and Monecillo,1983) Kenya (Raintress and Torres, 1986) Sumtra ( Sukmana et al.,1985) and Naigeria (Lal, 1989)
Run off control by alley cropping soon after pruning and planting (April May, 1986) IITA, Ibadan, Nigeria.
Treatment
|
Runoff
|
Relative runoff
|
Plowed control
|
99.5
|
100
|
No ill
|
10.3
|
10
|
Leucaena (4m)
|
26.6
|
27
|
Leucaena (2m)
|
9.0
|
9
|
Gliricidia (4m)
|
30.5
|
31
|
Gliricidia (2m)
|
27.8
|
28
|
(Source- R.Lal, 1990)
In brief, in Agroforestry, planting of closely spaced timbers and hedges create the barriers and reduce the runoff velocity. Closely spacing of trees allows more water to infiltrate, and as a result of this the surface runoff is decreased. Mulching with leaves and plastic helps to reduce the shit erosion. Since the soil is an important parameter in ecology, it has become important to look after soil erosion issue. There is again a good scope for erosion control technique in future.
Soil degradation can be prevened by soil water conservation methods such as formation of terraces, contour, graded bunds.etc. Along with this aforestration and water conservation methods also helps to reduce the soil erosion .Plantation of wind breaks cropping patterns, perennial plantations also stop soil erosion.
References-
1)Ziemer, Robert R. 1981. Keynote address, Theme 4, Management of steepland erosion: an overview. Journal Hydrology (N.Z.) 20(1): 8-16.
2) Agroforestry systems to control erosion on arable tropical steeplands.
R. Lal publication year 1990. (Page no-?)
3) Textbook, The nature and properties of soil Nyle C. Brady
Web sources.
http://www.unescap.org/stat/envstat/stwes-04.pdf (prepared by Dominic Ballayan, FAO)

