Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, 8360
Keszthely, Hungary
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Annamária Laborczi
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
András Makó
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, 8360
Keszthely, Hungary
Kálmán Rajkai
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
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Total article views: 4,657 (including HTML, PDF, and XML)
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This paper analyzes differences in the performance of the indirect and direct mapping method to derive 3-D soil hydraulic maps. Maps of saturated water content, field capacity and wilting point are presented for a 5775 km2 catchment at 100 m resolution. Advantages and disadvantages of the two methods are discussed. The absolute difference in soil water retention values is less than 0.025 cm3 cm−3 between maps derived with indirect and direct methods for 65–86 % of the catchment.
This paper analyzes differences in the performance of the indirect and direct mapping method to...
