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Effects of soil fertility and N application rates on soil organic N components and N mineralization
Received:March 18, 2025  Revised:June 04, 2025
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KeyWord:wheat;yield;N supply;N use efficiency;acid-soluble amino N
Author NameAffiliationE-mail
LIU Lin South Subtropical Crop Research Institute, China Academy of Tropical Agricultural Sciences/Key Laboratory of Tropical Crops Nutrition of Hainan Province, Zhanjiang 524091, China
Institute of Eco-Environment and Industrial Technology, Shanxi Agricultural University/Shanxi Province Key Laboratory of Soil Environment and Nutrient Resources, Taiyuan 030800, China
College of Life Science, Changzhi University, Changzhi 046000, China 
 
LI Puwang South Subtropical Crop Research Institute, China Academy of Tropical Agricultural Sciences/Key Laboratory of Tropical Crops Nutrition of Hainan Province, Zhanjiang 524091, China puwangli@163.com 
XU Minggang Institute of Eco-Environment and Industrial Technology, Shanxi Agricultural University/Shanxi Province Key Laboratory of Soil Environment and Nutrient Resources, Taiyuan 030800, China xuminggang@caas.cn 
MA Haiyang South Subtropical Crop Research Institute, China Academy of Tropical Agricultural Sciences/Key Laboratory of Tropical Crops Nutrition of Hainan Province, Zhanjiang 524091, China  
YANG Xueyun College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China  
ZHANG Shulan College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China  
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Abstract:
      To investigate the effects of soil fertility and fertilizer N application rates on organic N components and soil N supply capacity, optimize fertilizer N application and improve N use efficiency. Based on a N gradient micro-plot experiment established on plots subjected to various fertilization treatments for 26 years at a Loess soil, we systematically explored the wheat yield, above-ground N uptake, soil mineral N and organic N fractions under five soil fertility levels and at five N application rates, and aimed at established the correlation between organic N components and N mineralization. The result showed that the grain yield of winter wheat and N uptake of above-ground biomass significantly increased with increasing N application rate on low fertility soil, but showed no response to N rate on high fertility soil. Acid-soluble N(TNex)is the major form of soil organic N. The improvement of soil fertility level increased TNex content(691.07- 901.81 mg·kg-1), but decreased its proportion to total N(TN, 61.24%-78.57%), and increased the acid non-soluble N content(NHH, 221.46-587.38 mg·kg-1)and its proportion to TN(21.43%-38.76%). With the increase of soil fertility level, the content of acid-soluble hydrolysable unidentified N(HUN)was significantly decreased, and other organic N contents were significantly increased, especially so for the acid -soluble amino N(AAN). The proportions of ANN and HUN to TNex decreased with increasing soil fertility, whereas the proportion of AAN to TNex showed a concurrent increase with soil fertility levels. HUN was the main organic N fraction in low fertility soil (F1, F2), varying from 33.92% to 40.39%, while the major organic N fraction of high fertility soils(F3, F4 and F5)was AAN, ranging from 25.72% to 35.54%. The results of the Random Forest model showed that AAN had the highest relative importance for the apparent N mineralization, followed by the TNex, and that apparent N mineralization increased significantly with increasing AAN. N application rate had no significant effect on organic N components, but soil fertility level changed the distribution characteristics of organic N components in soil, and soil N supply capacity was mainly related to AAN. When soil AAN content arrived 494 mg·kg-1 and 439 mg·kg-1, wheat grain yield and above-ground N uptake maximum.