铝胁迫下硝普钠对黑麦和小麦根尖细胞壁铝吸附的影响

用一氧化氮供体硝普钠(sodium nitroprusside,SNP)处理铝胁迫下的黑麦和小麦幼苗,探讨铝胁迫和铝胁迫下外源NO对黑麦和小麦根尖细胞壁铝吸附的影响。结果表明:铝显著抑制黑麦和小麦根的伸长生长,小麦受抑制更为严重;SNP处理可缓解铝对黑麦和小麦根伸长生长的抑制作用,1 mmol/L SNP处理最有效。小麦根尖对铝的吸附量和吸附速率显著高于黑麦的,1 mmol/L SNP处理显著降低小麦和黑麦细胞壁对铝的吸附量,使根尖铝含量显著下降。铝与根尖细胞壁的结合是导致植物铝毒害的重要原因,而降低根尖细胞壁对铝的吸附是外源NO缓解铝毒害的重要机制。     

Fluxes of nitrous oxide and nitric oxide from experimental excreta patches in boreal agricultural soil

Nitric oxide (NO) and nitrous oxide (N₂O) emissions were measured from experimental dung and urine patches placed on boreal pasture soil during two growing seasons and one autumn period until soil freezing. N₂O emissions in situ were studied by a static chamber method. NO was measured with a dynamic chamber method using a NO analyser in situ. Mean emissions from the control plots were 47.6±4.5 μg N₂ON m⁻² h⁻¹ and 12.6±1.6 μg NON m⁻² h⁻¹. N₂O and NO emissions from urine plots (132±21.2 μg N₂ON m⁻² h⁻¹ and 51.9±7.6 μg NON m⁻² h⁻¹) were higher than those from dung plots (110.0±20.1 μg N₂ON m⁻² h⁻¹ and 14.7±2.1 μg NON m⁻² h⁻¹). There was a large temporal variation in N₂O and NO emissions. Maximum N₂O emissions were measured a few weeks after dung or urine application, whereas the maximum NO emissions were detected the following year. NO was responsible on average 14% (autumn) and 34% (summer) of total (NO+N₂O)N emissions from the pasture soil. NO emissions increased with increasing soil temperature and with decreasing soil moisture. N₂O emissions increased with increasing soil moisture, but did not correlate with soil temperature. Therefore we propose that N₂O and NO were produced mainly during different microbial processes, i.e., nitrification and denitrification, respectively. The results show that the overall conditions and mechanism especially for emissions of NO are still poorly understood but that there are differences in the mechanisms regulating N₂O and NO production.     

Nitrification controls N2O production rates in a frozen boreal forest soil

The winter season has been identified as a significant contributor to N₂O emissions from boreal soils, but our understanding of the processes regulating these emissions is fragmentary. We investigated potential N-sources and pathways involved in N₂O formation in a frozen boreal forest soil by labeling soil samples with ¹⁵N-containing substrates, and measured rates of ¹⁵N₂O/¹⁵N₂ formation under both oxic and anoxic conditions. Our results showed that all N₂O produced in the frozen samples originate from denitrification, but the rate-limiting factor is NO₃⁻ availability, which is largely governed by nitrification. This suggests that N₂O formation in frozen boreal soils may be sustained for a prolonged period of time, but is governed by a delicate balance of the O₂ regime.     

Dinitrogen and N2O emissions in arable soils: Effect of tillage, N source and soil moisture

A laboratory investigation was performed to compare the fluxes of dinitrogen (N₂), N₂O and carbon dioxide (CO₂) from no-till (NT) and conventional till (CT) soils under the same water, mineral nitrogen and temperature status. Intact soil cores (0-10 cm) were incubated for 2 weeks at 25 °C at either 75% or 60% water-filled pore space (WFPS) with ¹⁵N-labeled fertilizers (100 mg N kg⁻¹ soil). Gas and soil samples were collected at 1-4 day intervals during the incubation period. The N₂O and CO₂ fluxes were measured by a gas chromatography (GC) system while total N₂ and N₂O losses and their ¹⁵N mole fractions in the soil mineral N pool were determined by a mass spectrometer. The daily accumulative fluxes of N₂ and N₂O were significantly affected by tillage, N source and soil moisture. We observed higher (P<0.05) fluxes of N₂+N₂O, N₂O and CO₂ from the NT soils than from the CT soils. Compared with the addition of nitrate (NO₃⁻), the addition of ammonium (NH₄⁺) enhanced the emissions of these N and C gases in the CT and NT soils, but the effect of NH₄⁺ on the N₂ and/or N₂O fluxes was evident only at 60% WFPS, indicating that nitrification and subsequent denitrification contributed largely to the gaseous N losses and N₂O emission under the lower moisture condition. Total and fertilizer-induced emissions of N₂ and/or N₂O were higher (P<0.05) at 75% WFPS than with 60% WFPS, while CO₂ fluxes were not influenced by the two moisture levels. These laboratory results indicate that there is greater potential for N₂O loss from NT soils than CT soils. Avoiding wet soil conditions (>60% WFPS) and applying a NO₃⁻ form of N fertilizer would reduce potential N₂O emissions from arable soils.     

一氧化氮延缓草莓成熟衰老的生理效应

 以硝普钠（SNP）为一氧化氮（NO）供体，研究了不同浓度NO对丰香草莓采后果实乙烯产生、呼吸强度、维生素C（Vc）、可溶性蛋白、失水腐烂和相对电导率，以及超氧物歧化酶（SOD）、过氧化氢酶（CAT）和过氧化物酶（POD）活性的影响。结果表明，5 μmol·L-1 SNP释放NO可以抑制草莓果实乙烯的产生和呼吸强度，延缓乙烯产生和呼吸高峰的出现，并推迟了果实固酸比、Vc和可溶性蛋白含量下降时期，抑制果实腐烂失水和相对电导率升高；使果实CAT活性显著增强，SOD活性在后期高于对照，但POD活性低于对照。10 μmol·L-1 SNP对果实产生轻微毒害作用，1 μmol·L-1 SNP延迟草莓衰老的效果不明显。证明了NO抑制果实衰老与其浓度的相关性，揭示了NO保护细胞膜结构完整的作用机理。     

外源NO缓解果树胁迫的作用机理和研究进展

一氧化氮(Nitric oxide, NO)是一种重要的信号分子,广泛参与果树的生长发育调控和对生物与非生物环境胁迫的应答反应。大量证据表明,外源NO是缓解果树干旱、高温和酸雨等胁迫中重要的信使分子,其信号转导机制目前已广受人们关注。文章综述了NO的来源、NO的双重作用及作用机理、NO与其他信号分子间的关系以及近年来外源NO缓解果树胁迫的研究进展,为外源NO缓解果树胁迫的深入研究提供参考资料。     

嗜酸小球菌对凡纳滨对虾体液免疫因子的影响

在饲料中添加不同剂量的嗜酸小球菌投喂凡纳滨对虾,并在投喂后的20、40和60d,分别测定凡纳滨对虾血清中的一氧化氮合酶(NOS)、溶菌活力(Bacteriolytic activity)、总超氧化物歧化酶(T-SOD)、酸性磷酸酶(ACP)、碱性磷酸酶(AKP),并分析了这5种酶之间的相关性。结果显示,嗜酸小球菌能有效提高凡纳滨对虾体内的NOS、溶菌活力、T-SOD、ACP、AKP的活性;NOS与溶菌活力存在显著正相关性(P<0.05),与SOD存在显著负相关性,溶菌活力与AKP存在显著负相关性。表明在饲料中添加适量的嗜酸小球菌(剂量10mg/kg)可使凡纳滨对虾体液免疫因子活力到达较高的水平;凡纳滨对虾血清中一氧化氮合酶对于嗜酸小球菌的添加量较为敏感,可作为评价嗜酸小球菌使用效果的指标之一。     

一氧化氮合成酶(NOS)研究方法及其在植物中的应用

一氧化氮(NO)在动植物生命活动中具有重要作用。近年来,其合成途径已成为研究焦点。文章综述了近10年来一氧化氮合成酶(NOS)研究方法及其在植物中的应用,包括生物化学方法、免疫学方法和分子生物学方法,并对其研究前景进行展望。     

不同施肥和保水措施对油茶土壤N2O排放的影响

为探究不同施肥和保水措施对油茶土壤N_2O排放的影响,采用静态暗箱-气相色谱法,设置对照(B0CK)、氮肥(N,0.13 g N·kg~(-1))、磷肥(P,0.065 g P·kg~(-1))、氮磷肥(NP,0.13 g N·kg~(-1)+0.065 g P·kg~(-1))、低复合保水材料(生物炭和聚丙烯酰胺,B1,每盆13.65 g炭+1.35 g聚丙烯酰胺)、高复合保水材料(生物炭和聚丙烯酰胺,B2,每盆27.30 g炭+2.70 g聚丙烯酰胺)、低复合保水材料和N(NB1)、高复合保水材料和N(NB2)、低复合保水材料和P(PB1)、高复合保水材料和P(PB2)、低复合保水材料和NP(NPB1)、高复合保水材料和NP(NPB2),共12个处理,进行不同施肥和保水措施下土壤N_2O排放的差异比较。结果表明,N、P添加均显著增加土壤N_2O的累积排放量,NP添加与对照无差异。施加复合保水材料抑制土壤N_2O的排放,随着复合保水材料施用量的增加,土壤N_2O的排放显著降低,与对照相比,B1和B2处理N_2O减排50%以上。N添加条件下,与对照相比,添加复合保水材料NB1、NB2的N_2O累积排放显著降低。P与复合保水材料无交互作用。N、P和复合保水材料对土壤N_2O累积排放量具有显著作用,在NP同施时,与对照相比,添加复合保水材料NPB1、NPB2的N_2O累积排放分别降低了1.18%、30.69%。因此,高复合保水材料类型的施肥措施对减少油茶土壤N_2O排放具有重要意义,从而对缓解全球气候变化具有重要影响。     

Mitigating nitrous oxide emissions from agricultural soils by precision management

Nitrous oxide (N₂O) emissions make up a significant part of agricultural greenhouse gas emissions. There is an urgent need to identify new approaches to the mitigation of these emissions with emerging technology. In this short review four approaches to precision managements of agricultural systems are described based on examples of work being undertaken in the UK and New Zealand. They offer the opportunity for N₂O mitigation without any reduction in productivity. These approaches depend upon new sensor technology, modeling and spatial information with which to make management decisions and interventions that can both improve agricultural productivity and environmental protection.