Present addresses: Kitami Agricultural Experiment Station, AzaYayoi, Kunneppu, Hokkaido 099-1496, Japan.
Interpretation of soil mineral nitrogen by scoring organic matter and nitrogen management as an “N-score” in the fields of Hokkaido before sugar beet planting
Version of Record online: 25 NOV 2010
© 2010 Japanese Society of Soil Science and Plant Nutrition
Soil Science & Plant Nutrition
Volume 56, Issue 5, pages 750–759, October 2010
How to Cite
FUEKI, N., SATO, K. and NAKATSU, S. (2010), Interpretation of soil mineral nitrogen by scoring organic matter and nitrogen management as an “N-score” in the fields of Hokkaido before sugar beet planting. Soil Science & Plant Nutrition, 56: 750–759. doi: 10.1111/j.1747-0765.2010.00509.x
Okoppe Outstation of Monbetsu Branch Office, Hokkaido Abashiri Agricultural Extension Center, AzaOkoppe, Okoppe, Hokkaido 098-1612, Japan.
Central Agricultural Experiment Station, Naganuma, Hokkaido 069-1395, Japan.
- Issue online: 25 NOV 2010
- Version of Record online: 25 NOV 2010
- Received 10 March 2010. Accepted for publication 22 August 2010.
- field management;
- organic matter application;
- soil mineral nitrogen;
- soil nitrogen fertility
The objective of the present study was to investigate soil mineral nitrogen (N) in agricultural fields and to evaluate the factors that affect it. The amount of soil mineral N (0–100 cm depth) in 33 farming fields in the Hokkaido area, Japan, was investigated in April 2003, 2004 and 2005 (i.e. before sugar beet planting). The mean value and range of soil mineral N were 147 kg ha−1 and 44–750 kg ha−1, respectively. By analyzing six typical fields in detail (soil mineral N: 44–750 kg ha−1), we found that the history of organic matter application and other field management practices drastically affected the amount of soil mineral N. We referred to these histories and practices as “N-scores”. These scores take into account organic matter application and other field management practices by scoring N input using the Hokkaido Fertilizer Recommendations 2002. Soil mineral N was more closely related to the N-score (r = 0.839**, P < 0.01) than to other soil factors (e.g. pH, total C, total N, cation exchange capacity and autoclaved N). These results suggest that evaluating organic matter application and other field management practices by scoring N input (N-score) is useful not only for evaluating soil N fertility, which is expressed by soil mineral N, but also for estimating the risk of N leaching.