Evaluation of biological and chemical nitrogen indices for predicting nitrogen-supplying capacity of paddy soils in the Taihu Lake region, China

Li, W; Xia, Y; Ti, C; Yan, X

HERO ID

2051321

Reference Type

Journal Article

Year

2011

HERO ID 2051321
In Press No
Year 2011
Title Evaluation of biological and chemical nitrogen indices for predicting nitrogen-supplying capacity of paddy soils in the Taihu Lake region, China
Authors Li, W; Xia, Y; Ti, C; Yan, X
Journal Biology and Fertility of Soils
Volume 47
Issue 6
Page Numbers 669-678
Abstract Simple and rapid chemical indices of soil nitrogen (N)-supplying capacity are necessary for fertilizer recommendations. In this study, pot experiment involving rice, anaerobic incubation, and chemical analysis were conducted for paddy soils collected from nine locations in the Taihu Lake region of China. The paddy soils showed large variability in N-supplying capacity as indicated by the total N uptake (TNU) by rice plants in a pot experiment, which ranged from 639.7 to 1,046.2 mg N pot(-1) at maturity stage, representing 5.8% of the total soil N on average. Anaerobic incubation for 3, 14, 28, and 112 days all resulted in a significant (P < 0.01) correlation between cumulative mineral NH (4) (+) -N and TNU, but generally better correlations were obtained with increasing incubation time. Soil organic C, total soil N, microbial C, and ultraviolet absorbance of NaHCO(3) extract at 205 and 260 nm revealed no clear relationship with TNU or cumulative mineral NH (4) (+) -N. Soil C/N ratio, acid KMnO(4)-NH (4) (+) -N, alkaline KMnO(4)-NH (4) (+) -N, phosphate-borate buffer extractable NH (4) (+) -N (PB-NH (4) (+) -N), phosphate-borate buffer hydrolyzable NH (4) (+) -N (PB(HYDR)-NH (4) (+) -N) and hot KCl extractable NH (4) (+) -N (H(KCl)-NH (4) (+) -N) were all significantly (P < 0.05) related to TNU and cumulative mineral NH (4) (+) -N of long-term incubation (> 28 days). However, the best chemical index of soil N-supplying capacity was the soil C/N ratio, which showed the highest correlation with TNU at maturity stage (R = -0.929, P < 0.001) and cumulative mineral NH (4) (+) -N (R = -0.971, P < 0.001). Acid KMnO(4)-NH (4) (+) -N plus native soil NH (4) (+) -N produced similar, but slightly worse predictions of soil N-supplying capacity than the soil C/N ratio.
Doi 10.1007/s00374-011-0577-x
Wosid WOS:000292971700006
Url http://link.springer.com/10.1007/s00374-011-0577-x
Is Certified Translation No
Dupe Override No
Is Public Yes
Keyword Nitrogen-supplying capacity; Anaerobic incubation; Chemical indices; Paddy soils; Taihu Lake region