scholarly journals Nitrogen saturation, soil acidification, and ecological effects in a subtropical pine forest on acid soil in southwest China

2015 ◽  
Vol 120 (11) ◽  
pp. 2457-2472 ◽  
Author(s):  
Yongmei Huang ◽  
Ronghua Kang ◽  
Jan Mulder ◽  
Ting Zhang ◽  
Lei Duan
2016 ◽  
Vol 218 ◽  
pp. 1191-1199 ◽  
Author(s):  
Lei Duan ◽  
Xiao Chen ◽  
Xiaoxiao Ma ◽  
Bin Zhao ◽  
Thorjørn Larssen ◽  
...  

1999 ◽  
Vol 29 (5) ◽  
pp. 609-620 ◽  
Author(s):  
William S Currie ◽  
John D Aber ◽  
Charles T Driscoll

Nitrogen saturation results in greater mobility of nitrate, which in turn is often correlated with concentrations of nutrient cations in soil solution and streamwater. At the Harvard Forest, U.S.A., under long-term NH4NO3 inputs, a Pinus resinosa Ait. forest has exhibited signs of N saturation more rapidly than a mixed-Quercus forest. We test the hypothesis that increased nitrate leaching causes increased concentrations of nutrient cations in soil solution. Over 2 years (years 6 and 7 of treatment) we measured SO42-, NO3-, Cl-, Ca2+, K+, Mg2+, Na+, H+, and NH4+ in throughfall solution and in forest-floor (Oa) leachate. Concentrations of NO3- in forest-floor leachate increased with rates of N amendment and correlated positively with cation concentrations, with stronger overall correlations in the pine forest: r2 values were 0.51 (pine forest) and 0.39 (oak forest) for Ca2+, 0.45 (pine) and 0.16 (oak) for K+, and 0.62 (pine) and 0.50 (oak) for Mg2+. In summer and fall, the oak forest showed some negative relationships between nutrient cation leaching and rate of N amendment. These contrasts showed retention of cations and N to occur together in an N-limited system, whereas increased nitrate mobility occurred with increased cation losses in an N-saturated system.


2019 ◽  
Vol 25 (1) ◽  
pp. 31-40
Author(s):  
Mitsuhisa Baba ◽  
Masanori Okazaki ◽  
Kazuhide Matsuda ◽  
Emu Shima ◽  
Fuka Tachiyanagi ◽  
...  

2010 ◽  
Vol 10 (7) ◽  
pp. 1477-1485 ◽  
Author(s):  
M. Eidukeviciene ◽  
J. Volungevicius ◽  
S. Marcinkonis ◽  
L. Tripolskaja ◽  
D. Karcauskiene ◽  
...  

Abstract. An analysis of factors influencing effective soil acidification management is reported. This analysis was conducted simultaneously at both national and local levels. These investigations were accomplished in three stages: (i) validation of acid soil spatial patterns using systems analysis and geoinformation methods; (ii) spatial statistical analysis of soil pH diversity using a statistical grid method; and (iii) development of the concept of soil acidity management. Results indicate the national spatial distribution of topsoil reaction is a natural and stable phenomenon related to Quaternary sub-surface deposits. However, secondary effects of topsoil liming are evident in both spatial and temporal soil reaction patterns.


Sign in / Sign up

Export Citation Format

Share Document