『Abstract
Inorganic nitrogen deposition and leaching in stream water were
monitored from January, 2001 to December, 2004 in a subtropical
evergreen mixed forest in central-south China. The seasonal concentration
and flux of inorganic nitrogen in bulk precipitation and stream
water, seasonal mean net retention and stream water, seasonal
mean net retention of nitrogen and net flux of H+ transformed
by nitrogen were estimated and quantified in Shaoshan forest.
The research results show that the correlation coefficient of
fluxes between bulk precipitation and stream water is significant,
with a coefficient 0.916 at the 0.01 level. Mean flux of inorganic
nitrogen input are 2.62 g m-2 a-1 and 0.516
g m-2 a-1 in form of bulk precipitation
and dry deposition respectively, and output in stream water is
around 0.22 g m-2 a-1, which indicates that
most of nitrogen input is reserved in the forest. Net retention
of nitrogen reaches 2.916 m-2 a-1, just
higher than other study plots over the world. Along with the translating
of nitrogen (NH4+ - N and NO3- - N), H+ is imported
to the forest ecosystem at the same time. At our study plots,
net flux of H+ transformed by nitrogen is about 73.57
mmol m-2 a-1. The positive value suggests
that Shaoshan forest is still a finer buffering system to nitrogen
deposition and it is far from nitrogen saturation in spite of
the high nitrogen deposition.
Keywords: Concentration; flux; Inorganic nitrogen; Input-output;
Saturation』
1 Introduction
2 Materials and methods
2.1 Research site
2.2 Sampling design and laboratory analysis
2.3 Methodology
2.4 Study tentative
3. Results and discussions
3.1 Water fluxes and mean pH values in bulk precipitation
(BP) and stream water (SW)
3.2 Seasonal nitrogen concentrations in bulk precipitation and
stream water
3.3 Nitrogen fluxes in bulk precipitation and stream water in
Shaoshan forest during 2001-2004
3.4 Seasonal input-output budgets of inorganic nitrogen and net
flux of H+ translating by nitrogen in Shaoshan forest
3.5 Status of nitrogen saturation in Shaoshan forest
4 Conclusions
Acknowledgements
References
Country | Area | Years | Budget | ΔH+ | |||
Water (mm) | NH4+ - N | NO3- - N | NH4+ - N + NO3-b - N | ||||
China (This study) | Shaoshan | 2001-2004 | 789 | 1.973 | 0.943 | 2.916 | 73.57 |
Europaa (NITREX) | Sogndal | 1984-1992 | 46 | 0.126 | 0.089 | 0.215 | 2.64 |
Gardsjon(sの頭に゜、oの頭に¨) | 1989-1994 | 176 | 0.364 | 0.714 | 1.078 | -25 | |
Aber | 1991-1994 | 238 | 0.616 | -0.672 | -0.056 | 92 | |
Alptal | 1994 | 696 | 0.812 | 0.560 | 1.372 | 18 | |
Klosterhede | 1991-1994 | 354 | 0.910 | 0.924 | 1.834 | -1 | |
Solling | 1990-1994 | 344 | 1.750 | -0.364 | 1.386 | 151 | |
Speuld | 1990-1994 | 261 | 3.444 | -7.564 | -4.120 | 786.30 | |
Ysselsteyn | 1990-1994 | 303 | 4.494 | -5.515 | -1.021 | 714.90 | |
Japaneseb | SG-FC |
|
569 | 0.100 | 0.170 | 0.270 | -5 |
SG-FS | 569 | 0.110 | -0.010 | 0.100 | 8.57 | ||
SG-KR1 | 638 | 0.300 | 0.070 | 0.370 | 16.43 | ||
SG-KR2 | 706 | 0.170 | 0.250 | 0.420 | -5.72 | ||
SG-RO1 | 663 | 0.130 | 0.170 | 0.300 | -2.86 | ||
SG-RO2 | 675 | 0.150 | 0.180 | 0.330 | -2.14 | ||
SG-RO3 | 663 | 0.150 | 0.170 | 0.320 | -1.43 | ||
SG-RO4 | 649 | 0.040 | 0.250 | 0.290 | -15 | ||
KT-KM2 | 1043 | 0.180 | 0.110 | 0.290 | 5 | ||
SG-YT | 438 | 0.210 | 0.180 | 0.390 | 2.14 | ||
SG-SM1 | 1017 | 0.420 | 0.330 | 0.750 | 6.43 | ||
SG-AM2 | 1513 | 0.430 | 0.360 | 0.790 | 4.29 | ||
IG-TB | 842 | 0.500 | -0.720 | -0.220 | 87.14 | ||
GM-OS1 | 712 | >0.480 | -1.050 | -0.570 | 109.29 | ||
GM-OS2 | 660 | >0.480 | -0.790 | -0.310 | 90.72 | ||
HK-TEFD | 604 | 0.180 | 0.170 | 0.350 | 0.72 | ||
HK-TEFC | 682 | 0.090 | -0.160 | -0.070 | 17.86 | ||
United States | HBc | 1992-1993 | 482 | NA | NA | 0.664 | NA |
BBd,e | 1988-1990 | 492 | NA | NA | 0.113 | NA | |
CKf | 1985-1986 | 561 | NA | NA | 0.630 | NA | |
Budget = input - output, NA no data aBredemeier et al. 1998 bMitchell et al. 1997 cLikens and Bormann 1995 dKahl et al. 1993 eNorton et al. 1994 fStoddard and Murdoch 1991 |