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taungya in relation to soil properties soil erosion and soil management

taungya in relation to soil properties soil erosion and soil management

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21Soil <strong>erosion</strong> is a function of the erosivity of the ra<strong>in</strong> <strong>and</strong> the erodibility of <strong>soil</strong>.Erosivity is the potential ability of the ra<strong>in</strong> <strong>to</strong> cause <strong>erosion</strong> whereas erodibility isthe vulnerability of the <strong>soil</strong> <strong>to</strong> <strong>erosion</strong>. The latter depends on the <strong>in</strong>herentcharacteristics of the <strong>soil</strong> <strong>and</strong> how it is managed. In <strong>taungya</strong> plantations without<strong>soil</strong> conservation measures, both erosivity <strong>and</strong> erodibility are enhanced. Underrice-rice, rice-tapioca <strong>and</strong> tapioca cultivations, due <strong>to</strong> the additional <strong>soil</strong>disturbance <strong>in</strong> establish<strong>in</strong>g these crops, both these fac<strong>to</strong>rs are accelerated <strong>and</strong>therefore <strong>soil</strong> <strong>erosion</strong> occurs considerably more here than <strong>in</strong> the case of just ricecultivation.Soil ManagementThe experimental data po<strong>in</strong>t out the need for a different approach <strong>in</strong> the<strong>management</strong> of <strong>soil</strong>s <strong>in</strong> <strong>taungya</strong> plantations. If the forest l<strong>and</strong> is not properlymanaged <strong>in</strong> <strong>taungya</strong>, productive l<strong>and</strong> will be converted <strong>in</strong><strong>to</strong> unproductivemarg<strong>in</strong>al l<strong>and</strong>. This is ma<strong>in</strong>ly because the <strong>taungya</strong>dar has only a transient<strong>in</strong>terest <strong>in</strong> the area he cultivates or gets it cultivated. Two years of cultivationwithout proper <strong>soil</strong> <strong>management</strong> practices can convert an area <strong>in</strong><strong>to</strong> anunproductive one. Also permanent damages occur <strong>in</strong> our <strong>taungya</strong> plantations. For<strong>in</strong>stance, comb<strong>in</strong>ed use of l<strong>and</strong> for agriculture <strong>and</strong> silviculture is oftendetrimental <strong>to</strong> forest plantations, especially on slopy areas. Also the exposure<strong>and</strong> loss of <strong>to</strong>p<strong>soil</strong> can lead <strong>to</strong> <strong>in</strong>creased laterization which results <strong>in</strong> theformation of a hard surface layer or a hard crust on the surface of the <strong>soil</strong>.The data tend <strong>to</strong> show that one crop of rice causes m<strong>in</strong>imum changes whereasrice-rice, rice-tapioca <strong>and</strong> tapioca cultivations cause maximum changes <strong>in</strong> someof the <strong>soil</strong> <strong>properties</strong>. The advantage of one rice crop is that it causes m<strong>in</strong>imumdisturbance <strong>to</strong> the surface horizons of the <strong>soil</strong>s. After the harvest, the residuesform a surface much which will retard runoff <strong>and</strong> <strong>erosion</strong>.Soil <strong>management</strong> practices <strong>to</strong> combat <strong>soil</strong> <strong>erosion</strong> are generally based on twobroad pr<strong>in</strong>ciples; firstly, practices which <strong>in</strong>crease <strong>in</strong>filtration rates of <strong>soil</strong>s forreduc<strong>in</strong>g runoff <strong>and</strong> secondly, practices which help safe disposal of runoff water ifra<strong>in</strong>fall exceeds the <strong>in</strong>filtration capacity of the <strong>soil</strong>s. Usually a comb<strong>in</strong>ation ofboth practices are essential for adequate <strong>erosion</strong> control. Practices which help <strong>to</strong>ma<strong>in</strong>ta<strong>in</strong> high <strong>soil</strong> <strong>in</strong>filtration rates are based on farm<strong>in</strong>g operations which willma<strong>in</strong>ta<strong>in</strong> a mulch or vegetative cover on the <strong>soil</strong>. The safe disposal of runoffwater requires physical manipulation of l<strong>and</strong> <strong>in</strong>clud<strong>in</strong>g l<strong>and</strong>shap<strong>in</strong>g, lay<strong>in</strong>g out ofcon<strong>to</strong>ur bunds, terraces, waterways, <strong>and</strong> ridges. Consider<strong>in</strong>g the constra<strong>in</strong>t off<strong>in</strong>ancial resources <strong>in</strong> lay<strong>in</strong>g out eng<strong>in</strong>eer<strong>in</strong>g control methods, the least we canfollow is the use of crop residues from the previous crop for conservation of <strong>soil</strong>.As suggested before, the residues left after the harvest of first rice crop form asurface mulch which prevents direct ra<strong>in</strong>drop impact on the <strong>soil</strong>. Because there ism<strong>in</strong>imum tillage, it decreases runoff <strong>and</strong> reduces <strong>soil</strong> loss. Further, such a mulchreduces weed growth <strong>and</strong> conserves moisture <strong>in</strong> the <strong>soil</strong> profile.

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