000 031820000a22005530004500
999 _c51189
_d51189
003 CR-TuBCO
005 20210628140214.0
007 ta
008 210628t 1986 ||||| |||| 00| 0 eng d
040 _aCR-TuBCO
_cCR-TuBCO
_bEspañol
041 0 _aeng
100 1 _995324
_aMontagnini, F.
100 1 _975620
_aHaines, B.
100 1 _950207
_aBoring, L.
100 1 _9122556
_aSwank, W.
245 1 0 _aNitrification potentials in early successional black locust and in mixed hardwood forest stands in the Southern Appalachians, USA
260 _aAmsterdam (Países Bajos):
_bSpringer,
_c1986
270 _aSan José, C.R.
300 _a14 páginas:
_b4 tablas
504 _aIncluye referencias bibliográficas en las páginas 209-210
520 _aSoil nitrogen mineralisation and nitrification potentials, and soil solution chemistry were measured in black locust (Robinia pseudo-acacia L.), in pine-mixed hardwood stands on an early successional watershed (WS6), and in an older growth oak-hickory forest located on an adjacent, mixed hardwood watershed (WS14) at Coweeta Hydrologic laboratory, in the southern Appalachian mountains, U.S.A. Nitrification potentials were higher in black locust and pine-mixed hardwood early successional stands than in the oak-hickory forest of the older growth watershed. Ammonification rates were the main factor controlling nitrification in the early successional stands. There was no evidence of inhibition of nitrification in soils from the older growth oak-hickory forest site. Within the early successional watershed, black locust sites had net mineralisation and nitrification rates at least twice as high as those in the pine mixed-hardwood stands. Concentrations of exchangeable nitrate in the soil of black locust stands were higher than in pine-mixed hardwoods at 0–15 cm in March and they were also higher at 0–15, 16–30 and 31–45 cm depth in the black locust dominated sites in July. Soil solution nitrate concentrations were higher under black locust than under pine-mixed hardwoods. Areas dominated by the nitrogen fixing black locust had greater nitrogen mineralisation and nitrification rates, resulting in higher potential for leaching losses of nitrate from the soil column in the early successional watershed.
650 1 4 _9163306
_aROBINIA PSEUDOACACIA
650 1 4 _9147945
_aFIJACION DEL NITROGENO
650 1 4 _9165569
_aSUELO
650 1 4 _9141440
_aCOMPOSICION QUIMICA
650 1 4 _9138269
_aBOSQUE MIXTO
650 1 4 _924573
_aEUA
691 _9163306
_aROBINIA PSEUDOACACIA
691 _aNITROGEN FIXATION
691 _9165084
_aSOIL
691 _9310534
_aCHEMICAL COMPOSITION
691 _9327454
_aMIXED FORESTS
691 _aUSA
_xUSA
773 0 _tBiogeochemistry (Países Bajos)
_gVolumen 2, páginas 197-210
_d1986
856 4 0 _uhttps://doi.org/10.1007/BF02180195
_qpdf
_yeng
904 _aBCO
904 _aacarvajal
905 _aC
906 _b20111124
907 _a000006625
907 _a000005196
907 _a000007156
907 _a000001794
907 _a000004874
907 _a000008114
908 _aJ
942 _cDIG
_2z