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1.
Abstract. Nitrous oxide (N2O) is involved in both ozone destruction and global warming. In agricultural soils it is produced by nitrification and denitrification mainly after fertilization. Nitrification inhibitors have been proposed as one of the management tools for the reduction of the potential hazards of fertilizer-derived N2O. Addition of nitrification inhibitors to fertilizers maintains soil N in ammonium form, thereby gaseous N losses by nitrification and denitrification are less likely to occur and there is increased N utilization by the sward. We present a study aimed to evaluate the effectiveness of the nitrification inhibitor dicyandiamide (DCD) and of the slurry additive Actilith F2 on N2O emissions following application of calcium ammonium nitrate or cattle slurry to a mixed clover/ryegrass sward in the Basque Country. The results indicate that large differences in N2O emission occur depending on fertilizer type and the presence or absence of a nitrification inhibitor. There is considerable scope for immediate reduction of emissions by applying DCD with calcium ammonium nitrate or cattle slurry. DCD, applied at 25 kg ha–1, reduced the amount of N lost as N2O by 60% and 42% when applied with cattle slurry and calcium ammonium nitrate, respectively. Actilith F2 did not reduce N2O emissions and it produced a long lasting mineralization of previously immobilized added N.  相似文献   
2.
研究旨在分析土壤中可培养细菌菌株的氮代谢特征,并进一步探讨微生物在土壤氮素转化中的可能作用机制。以2株分离自苹果园土壤的细菌菌株SY5-4和SY11-10为试材,采用传统培养方法结合分子检测技术,分别测定菌株生长特性及其氮素转化能力。研究结果表明,异养条件下,菌株SY5-4和SY11-10的世代时间分别为243.5 min和202.7 min。菌株生长过程中,培养液中铵态氮浓度始终维持在较高水平,铵态氮、亚硝态氮和硝态氮浓度均表现出先升后降的趋势。硝化(amoA和hao)和反硝化(nosZ、norB、nirK和nap)基因检测结果表明,菌株SY11-10具有多种氮素转化潜能。综上,供试菌株培养过程中,培养液中氮素发生变化,并在菌体中检测到不同氮转化基因,表明菌株参与多种氮代谢途径。  相似文献   
3.
Nitrification plays a central role in global nitrogen cycle, which is affected by biological interaction between soil microfauna and microorganisms. However, the complexity of soil biotic communities made it difficult to reveal organizational principles of the community and the interactions among species. Here, we used the network analysis to decipher the interactions between nematodes and ammonia oxidizers within aggregate fractions under 10-year manure application, and examine their associations with soil variables and potential nitrification activity (PNA). Three aggregate fractions included large macroaggregates (>2000 μm, LA), small macroaggregates (250–2000 μm, SA), and inter-aggregate soil and space (<250 μm, IA). Aggregate factions showed a remarkable effect on association networks of nematodes and ammonia oxidizers. The average connectivity (avgK) and the number of edges in overall networks increased with increasing aggregate sizes, while the average geodesic distance (GD) followed the opposite trend. The LA network could be viewed as a better organized or a better operational soil food web with more functional interrelated members than the SA and IA networks. The modules related to PNA were significantly correlated and clustered together as meta-modules in networks of aggregate fractions. The role-shifts prevailed among the network members such as significant module memberships (MMs) and generalist/specialist operational taxonomic units (OTUs). A half of shared nodes were further identified as shared MMs, dominated by ammonia-oxidizing bacteria (AOB) especially for Nitrosospira cluster 3a and 10. Soil pH could explain partly the shift of module hubs in different networks, while grazing by bacterivores might account for three exclusively connecters related to Nitrososphaera clusters 1.1. The strongly coupled modules correlated positively to pH and total carbon (TC), regardless of aggregate fractions. The network analysis approach provided new insights into potential importance of network interactions between nematodes and ammonia oxidizers in soil nitrogen cycling.  相似文献   
4.
硝、铵态氮肥对旱地土壤氧化亚氮排放的影响   总被引:5,自引:0,他引:5  
用静态箱法在田间研究了黄土性土壤不同水分条件下施用硝态氮肥和铵态氮肥后土壤N2O的排放特点,并对包括温度、pH、水分等因子的影响进行了探讨.结果表明:在水分含量为田间持水量的90%和70%的条件下,铵态氮肥处理土壤的平均N2O排放量分别为233.6±165.4 μg/(m2·h)和166.4±153.3 μg/(m2·h);而施用硝态氮肥时则仅为75±40.2 μg/(m2·h)和49.27±17.0 μg/(m2·h).施肥后短期内,铵态氮肥排放的N2O量显著高于硝态氮肥处理,由此可说明黄土性土壤表层土壤N2O的主要来源是土壤氮的硝化过程.在自然矿化条件下黄土性土壤N2O的排放量约为17.0 μg/(m2·h).如果把两个水分处理相比较,土壤水分对铵态氮肥处理土壤N2O的排放影响不明显,而对施用硝态氮肥的土壤有明显影响,高水分处理更利于土壤反硝化作用的进行从而增加了土壤N2O的排放量.施用不同肥料种类在施肥后短期内影响土壤的pH值和有效NO-3-N、NH 4-N含量,而反过来土壤水分含量、土壤pH以及土壤温度均不同程度地影响着土壤N2O的产生和排放.  相似文献   
5.
Vegetable soils with high nitrogen input are major sources of nitrous oxide (N2O) and nitric oxide (NO), and incorporation of the nitrification inhibitor 3, 4-dimethylpyrazole phosphate (DMPP) into soils has been documented to effectively reduce emissions. However, the efficiency of DMPP in terms of soil N2O and NO mitigations varies greatly depending on soil temperature and moisture levels. Thus, further evaluations of DMPP efficiency in diverse environments are required to encourage widespread application. A laboratory incubation study (28 d) was established to investigate the interactive effects of DMPP, temperature (15, 25, and 35 ℃), and soil moisture (55% and 80% of water-holding capacity (WHC)) on net nitrification rate, N2O and NO productions, and gene abundances of nitrifiers and denitrifiers in an intensive vegetable soil. Results showed that incubating soil with 1% DMPP led to partial inhibition of the net nitrification rate and N2O and NO productions, and the reduction percentage of N2O production was higher than that of NO production (69.3% vs. 38.2%) regardless of temperature and soil moisture conditions. The increased temperatures promoted the net nitrification rate but decreased soil N2O and NO productions. Soil moisture influenced NO production more than N2O production, decreasing with the increased moisture level (80%). The inhibitory effect of DMPP on cumulative N2O and NO productions decreased with increased temperatures at 55% WHC. Conversely, the inhibitory effect of DMPP on cumulative N2O production increased with increased temperatures at 80% WHC. Based on the correlation analyses and automatic linear modeling, the mitigation of both N2O and NO productions from the soil induced by DMPP was attributed to the decreases in ammonia-oxidizing bacteria (AOB) amoA gene abundance and NO-2-N concentration. Overall, our study indicated that DMPP reduced both N2O and NO productions by regulating the associated AOB amoA gene abundance and NO-2-N concentration. These findings improve our insights regarding the implications of DMPP for N2O and NO mitigations in vegetable soils under various climate scenarios.  相似文献   
6.
通过两年田间定位试验,探讨脲酶/硝化抑制剂配施氮肥在黑土区玉米体系中的氨减排及氮素增效效果。设置两种耕作模式(条耕和旋耕)和3种氮肥类型(常规尿素、添加脲酶抑制剂尿素、添加硝化抑制剂尿素)。结果表明,条耕产量和氮素利用率分别为8 631 kg/hm2和33.4%,明显低于旋耕;氨挥发总量为20.6 kg/hm2,明显高于旋耕。脲酶/硝化抑制剂配施氮肥的产量和氮素利用率分别为10 737 kg/hm2和46.0%,较常规尿素分别提高25.6%和23.6%;土壤氨挥发累积量为18.6 kg/hm2,明显低于常规尿素。抑制剂类型显著影响氨排放,添加脲酶抑制剂尿素低于添加硝化抑制剂尿素。相同氮素投入条件下,添加脲酶/硝化抑制剂尿素在土壤条耕和旋耕模式下均可实现增产增效及氨减排效果,且添加脲酶抑制剂尿素具有较好的氨减排效果。  相似文献   
7.
1,9-癸二醇是由水稻根系分泌物中发现的一种新型生物硝化抑制剂,在农业生产中可提高氮肥利用率,减少氮素损失。为建立一套超声波提取-气相色谱检测土壤中1,9-癸二醇的方法,分别对超声波提取条件(提取剂、提取次数、液料比、超声时间)和气相色谱检测参数(进样口温度、检测器温度、升温程序)进行研究。结果表明,超声波提取土壤1,9-癸二醇的最佳方法为甲醇作为提取剂超声提取1次,液料比40mL·g~(–1),超声时间30 min。气相色谱Agilent8890测定1,9-癸二醇的最佳条件为进样口温度250℃;氢火焰离子化检测器(FID)温度310℃;升温程序:初始柱温60℃,保持2 min,以20℃·min~(–1)的速率升至150℃,然后以3℃·min~(–1)的速率升至180℃,保持2 min,最后以20℃·min~(–1)的速率升至270℃。在最佳提取和测定条件下,不同浓度1,9-癸二醇的加标回收率为90.58%~94.55%。超声提取-气相色谱法检测限低、灵敏度和精密度高,快速高效、重复性好,为今后1,9-癸二醇的实际应用工作奠定了基础。  相似文献   
8.
上海城郊不同农业用地类型土壤硝化和反硝化作用   总被引:5,自引:0,他引:5  
采用气压过程分离(BaPS)技术对上海城郊不同农业用地类型土壤总硝化速率和反硝化速率进行了测定.结果表明:不同农业用地类型土壤总硝化速率和反硝化速率差异显著(p<0.05).其中大棚蔬菜总硝化速率和反硝化速率最高;在土壤含水量15%~30%范围内.土壤总硝化作用和反硝化作用对氮损失的贡献率分别为46.8%,53.2%.土壤含水量和土壤通气孔隙度的适度增加均有利于土壤硝化作用和反硝化作用的进行;总硝化速率与土壤含水量、土壤通气孔隙度、全氮含量呈显著性相关(p<0.05),与土壤N_3~--N呈极显著性相关(p<0.01);反硝化速率与土壤含水量、N_3~--N、全氮呈显著性相关(p<0.05),与土壤通气孔隙度呈极显著性相关(p<0.01);中等土壤含水量范围内,影响土壤硝化作用、反硝化作用的环境因子趋于多样和复杂化,各种土壤环境因子共同影响和决定土壤硝化和反硝化过程.  相似文献   
9.
采用原状土柱模拟方法,探讨了施肥水平、添加不同碳氮比(C/N)有机物、不同类型土壤、土壤水分含量及温度对含3,4-二甲基吡唑磷酸盐(3,4-dimethyl pyrazole phosphate,DMPP)硝化抑制剂的尿素(DMPP尿素)氨挥发损失的影响。结果表明,施肥水平对DMPP尿素的氨挥发损失有显著影响,随着DMPP尿素施用量的增加,土壤氨挥发损失量呈显著上升的趋势;DMPP尿素配施低C/N比的有机物鸡粪,氨挥发损失增加6.0%;而配施高C/N比的生物秸秆,则表现为可抑制78.2%的氨挥发损失;DMPP尿素的氨挥发损失受土壤理化性质影响很大,在肥力高的碱性土壤中氨挥发损失严重,而在酸性红壤和阳离子交换量高的青紫泥中挥发损失量较低;在土壤含水量为田间饱和持水量时,氨挥发损失表现为急剧增加;随着土壤温度的升高,氨挥发损失的量快速递增。合理控制施肥量、选择配施高C/N比的生物秸秆和适宜的水分管理方式是减少农田氨挥发损失的重要对策。  相似文献   
10.
矿化作用和硝化作用是土壤氮素转化的主要途径,通过室内培养试验,对设施和露天栽培方式下有机菜地土壤氮素的矿化与硝化作用进行了比较研究。结果表明,除培养第1d外,设施有机菜地土壤氮素矿化量、矿化率在整个培养期间都显著高于露天有机菜地土壤;设施有机菜地土壤硝化量、硝化率在培养前两周内高于露天有机菜地土壤;设施有机菜地土壤矿化与硝化作用总体比露天有机菜地土壤强烈。矿化作用可能与全氮、C/N、微生物活性关系密切,而硝化作用强弱可能与微生物活性有关。无论施肥与否,设施有机菜地土壤N2O排放速率在培养期间总体高于露天有机菜地土壤,前者N2O累积排放量显著高于后者,这可能与土壤C/N有关。  相似文献   
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