LNS18 College on Soil Physics

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Maktav, H. Erol, F. S. Erbek, D. Okçu, A. S. Sogut, P. Giacomich, S. Mauro, K. Mighozzi, (2002) “The Use of Conventional Data and Remote Sensing for Classification of Erosion and Land Degradation”, 3rd. AGROENVIRON Symposium, 26-28 October, Cairo. C and J. 131. , (1993) The USLE for Predicting Rainfall Erosion Losses. ICTP-SMR. 705-3. Trieste, Italy. , and R. Francisco, 2000- Evaluating uncertainties in prediction of regional climate changing. Geophysical letters, Vol. 27, No. 9, pp. 1295-1298.

Giorgi and the Climate Impacts LINK project members for gridded data supporting. REFERENCES Aslan, Z, (1997) Analysis of Rainfall Erosivity and Climatic Factor of Wind Erosion. ICTP Pre-print, IC/97/135, Trieste, Italy. , and A. Tokgözlü, (2000) Climatological Changing Effects on rainfall Erositivty and Wind Erosion”, AGROENVIRON2000: 2nd. 265-273. , E. Skidmore, E. Feoli, D. Maktav, H. Erol, F. S. Erbek, D. Okçu, A. S. Sogut, P. Giacomich, S. Mauro, K. Mighozzi, (2002) “The Use of Conventional Data and Remote Sensing for Classification of Erosion and Land Degradation”, 3rd.

And Moody, K. 1999b. Water, tillage and weed management options for wet seeded rice in the Philippines. K. M. 1993. Puddling and compaction effects on water permeability of texturally different soils. J. Indian soc. Soil Sci. 41: 1-6. S. M. 1995. Soil structural improvements with addition of Lantana camara biomass in rice-wheat cropping. Soil Use and Management, 11: 199-203. 54 Table 1. 15 m depth under various treatments. K. D. M. 15 m) depth in a wet season. 18x10-6 *DS = Dry conventionally tilled plots; DS+H = Dry conventionally tilled plots followed by wet tillage (Halod) at 3-4 leaf stage of rice; DS+FYM = Dry conventionally tilled plots supplied with 10 t ha-1 farm yard manure; C = Soil compaction; RF = Ridge furrow system; P+TP = Puddling and transplanting Treatment* Bulk density (Mg m-3) Soil penetration resistance (MPa) Rice Lands of South & South East Asia, Some Soil Physical Aspects Table 2.

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