. . . . "28"^^ . "The \u010Certovo watershed (CT) is covered with ~0.5 m deep spodo-dystric cambisol (58%) and podzol (21%), and shallow (~0.2 m) undeveloped organic rich soil (17%). Similar contribution of soil types is in the \u010Cern\u00E9 watershed (CN). Fine soil is sandy (48-81%), with a low (1-4%) content of clay, and its watershed weighted mean (WWM) pool is 225 and 143 kg/m2 in the CT and CN. The WWM element pools in the CT and CN are (all in mol/m2): C, 1350 and 1120; N, 59 and 50; P, 5.4 and 3.4; and S, 2.8 and 2.6. Soil pH is lowest (2.5-3.3) in the A and highest (3.6-4.5) in the C horizons. The WWM cation exchange capacity is 104 and 123 meq/kg (with base saturation of 9% and 12%) in CT and CN, resp., and is dominated by exchangeable Al (62% and 55%). Concentrations of C, N, and P in soil microbial biomass are 0.3-1.4%, 2-4%, and 1-15% of their total contents. Moreover, data on C and N mineralization rate, nitrification potential, and extractable Fe, Al, P, and S, are reported." . "RIV/60077387:_____/02:62023139" . "P(GA206/00/0063), Z(AV0Z6017912), Z(AV0Z6066911), Z(MSM 123100004)" . . . . "Silva Gabreta" . "Physical, chemical, and biochemical characteristics of soils in watersheds of the Bohemian Forest lakes: II. \u010Certovo and \u010Cern\u00E9 Lakes."@en . . "Ka\u0148a, J." . "Physical, chemical, and biochemical characteristics of soils in watersheds of the Bohemian Forest lakes: II. \u010Certovo and \u010Cern\u00E9 Lakes."@en . . "Physical, chemical, and biochemical characteristics of soils in watersheds of the Bohemian Forest lakes: II. \u010Certovo and \u010Cern\u00E9 Lakes." . "Picek, T." . "Hejzlar, Josef" . "67;94" . "Physical, chemical, and biochemical characteristics of soils in watersheds of the Bohemian Forest lakes: II. \u010Certovo and \u010Cern\u00E9 Lakes." . . "Kop\u00E1\u010Dek, Ji\u0159\u00ED" . . "CZ - \u010Cesk\u00E1 republika" . "3"^^ . "Vesel\u00FD, J." . "658260" . "acidity; soil"@en . "1211-7420" . . "0"^^ . "[AD005F196712]" . "0"^^ . "The \u010Certovo watershed (CT) is covered with ~0.5 m deep spodo-dystric cambisol (58%) and podzol (21%), and shallow (~0.2 m) undeveloped organic rich soil (17%). Similar contribution of soil types is in the \u010Cern\u00E9 watershed (CN). Fine soil is sandy (48-81%), with a low (1-4%) content of clay, and its watershed weighted mean (WWM) pool is 225 and 143 kg/m2 in the CT and CN. The WWM element pools in the CT and CN are (all in mol/m2): C, 1350 and 1120; N, 59 and 50; P, 5.4 and 3.4; and S, 2.8 and 2.6. Soil pH is lowest (2.5-3.3) in the A and highest (3.6-4.5) in the C horizons. The WWM cation exchange capacity is 104 and 123 meq/kg (with base saturation of 9% and 12%) in CT and CN, resp., and is dominated by exchangeable Al (62% and 55%). Concentrations of C, N, and P in soil microbial biomass are 0.3-1.4%, 2-4%, and 1-15% of their total contents. Moreover, data on C and N mineralization rate, nitrification potential, and extractable Fe, Al, P, and S, are reported."@en . "RIV/60077387:_____/02:62023139!RIV/2003/GA0/A62003/N" . "Porcal, Petr" . . . . . "8"^^ . . . "N/A" . "\u0160antr\u016F\u010Dkov\u00E1, Hana" . . "8" . . "\u0160imek, Miloslav" .