Short communicationDoes the incorporation of dicyandiamide and hydroquinone with straw enhance the nitrogen supplying capacity in soil?
Introduction
Soil microorganism is the primary driving agent of nitrogen (N) cycling and an important N sink and source for crops (Nannipieri and Paul, 2009). To regulate N cycling, many researchers improve microbial activity by adding organic materials (Chen et al., 2014). The fixation and defixation of ammonium by soil clay minerals are also important processes for N cycling in soils, especially in 2:1 clay minerals (Nieder et al., 2011). More than 70% of applied fertilizer N can be fixed in some types of soil, and over 80% of recently fixed NH4+ can be released after several weeks or during growing seasons (Ahmad et al., 1982, Matsuoka and Moritsuka, 2011). However, less attention has been given to the comparison between the effects of soil microbial biomass N (SMBN) pool on N conservation and supply and those of fixed NH4+ pool.
For the amelioration of N use efficiency (NUE) and mitigation of environmental pollution, fertilizer N transformation processes in soil are usually regulated with inhibitors (Abalos et al., 2014), which alter the form of fertilizer N by retarding ammonium oxidation (nitrification inhibitors) or urea hydrolysis (urease inhibitors). The cationic form of fertilizer N can be enhanced and retained through inhibitor additions, which is the preferred source of N for microorganisms (Jansson, 1958) and can be fixed by soil clay minerals (Nieder et al., 2011). Kaye and Hart (1997) inferred that the competition for NH4+ exists between microbial activity (immobilization or nitrificaton) and mineral fixation processes. Microbial activity is also a primary driving force of fixed NH4+ release, and NH4+ derived from organic N mineralization can be fixed by clay minerals (Nieder et al., 2011, Ma et al., 2015). Therefore, the relationship between SMBN and fixed NH4+ pools should be clarified for the assessment of N availability and optimization of N management.
In the present study, a pot experiment was carried out with inhibitors and straw additions. The objectives were as follows: (i) to elucidate the synergistic effects of nitrification inhibitor (dicyandiamide, DCD), urease inhibitor (hydroquinone, HQ), and straw on N transformation; (ii) to compare the contributions of the SMBN and fixed NH4+ pools to N supply; and (iii) to identify the effects on crop yield.
Section snippets
Experimental site, design, and treatments
Test soil (0–10 cm) without fertilization since 1990 was collected from a long-term experiment in Shenyang Experimental Station, Chinese Academy of Sciences. The study area and the test soil properties were described in detail by Ma et al. (2015).
The pot experiment was conducted with spring wheat (Triticum aestivum L.) from April 6 to July 4, 2013 in a net house, which was furnished with a rainproof shelter. Nine treatments were performed, namely, (1) control (CK), (2) urea (U), (3)
Result
Soil mineral N (NH4+-N plus NO3−-N) was significantly influenced by the inhibitors and straw additions (Fig. 1a, b). In the absence of straw, the NH4+-N levels in the treatments that received DCD remained high relative to that in the U treatment. The SMBN and fixed NH4+ increased respectively by 4.0 mg kg−1 (25.5%) and 15.7 mg kg−1 (7.4%) in the DCD treatment and 6.2 mg kg−1 (39.3%) and 4.1 mg kg−1 (1.9%) in the DCD + HQ treatment, compared with the U treatment (Fig. 1c, d). However, the peaks
Discussion
Nitrogen was immobilized in the present study by microorganism approximately equal to 16.4% of the applied fertilizer N in the treatments without straw. Both inhibitors raised the average level of SMBN, especially when DCD was coupled with HQ. Xu et al. (2001) obtained parallel result and pointed out that inhibitors, particularly DCD, prolong the presence of NH4+, facilitating microbial immobilization (Jansson, 1958). When straw was applied, SMBN significantly increased, accounting for 39.0% of
Conclusion
In the absence of straw, inhibitor addition increased N supplying capacity in soil and crop yield. The most evident increase was observed when both HQ and DCD were used. The addition of straw, along with DCD, significantly decreased N supply in current season and crop yield. The decreases were attributed to drastic microbial immobilization and subsequent slow remineralization, which weakened the synchrony of the N supply with crop demand. However, urease inhibitor can be utilized for the
Acknowledgements
This work was financially supported by the National Natural Science Foundation of China (grant numbers 41471250, 41877106, 41877107), National Key Technology R&D Program (grant number 2015BAD05B01), and Doctoral Research Fund of Liaoning Province, China (grant number 20180540071).
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