硼酸共沉淀法合成含硼氧化铁的结构状况解析     

阎华  吴传兵  刘慧红  林淦 《土壤》2007,39(4):643-645

在水合法制备针铁矿过程中添加HBO3,对合成的样品作红外光谱和比表面积分析.结果表明,共沉淀法合成的样品在1343 cm处有特征吸收峰,说明在针铁矿形成过程中,如果有H3BO3参与,则形成的氧化铁中存在Fe-O-B键结构,可能在氧化铁内部有一种新硼铁化合物生成.比表面积测定表明,含B氧化铁比表面积增加4倍以上,反映了氧化铁与H3BO3并非机械混合物,其表面性质因为Fe与B反应而发生改变,B阻止氧化铁向高聚合态转变.  相似文献   

不同浓度钙营养液对烟草矿质营养吸收与积累的影响   总被引：9，自引：1，他引：9  

介晓磊  刘世亮  李有田  化党领  黄元炯  刘国顺  张弘韬 《土壤通报》2005,36(4):560-563

本文采用温室水培的方法,研究了不同的钙素供应水平对烟草各种矿质养分的吸收与积累的影响。结果表明,在其它养分形态与浓度一致条件下,随着钙浓度从75mgL-1提高到900mgL-1,烟草生长量呈抛物线型变化。钙浓度为150mgL-1时烟株干物质量最大。超过150mgL-1,随钙的增加而下降,当钙素达900mgL-1(K/Ca为1/6)时,烟株生长严重受抑。随着供钙水平由低到高,烟株氮、磷、钾、锌、锰含量均呈抛物线型变化,含钙量呈直线上升关系,而镁和铜含量则随钙浓度提高而显著下降。烟株各养分积累量均随营养液钙浓度提高呈抛物线型变化,但不同养分出现最大积累量时的营养液钙浓度却不相同。不同供钙水平上烟叶中各元素含量的变化特征与全株的结果基本一致。在低钙浓度范围(75~300mgL-1),钙对钾有协合关系,增钙促进提钾,大于300mgL-1后有拮抗作用,提钙导致降钾。钙与镁、锌、铜、锰间也存在明显的交互作用。烟叶中各元素含量与积累量的变化趋势与整株基本一致。  相似文献   

铝胁迫下硝普钠对黑麦和小麦根尖细胞壁铝吸附的影响     

何虎翼  何龙飞  黎晓峰  顾明华 《广西农业生物科学》2007,26(3):235-239,249

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。  相似文献   

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

Marja Maljanen  Mika Martikkala  Perttu Virkajärvi 《Soil biology & biochemistry》2007,39(4):914-920

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.  相似文献   

Nitrification controls N₂O production rates in a frozen boreal forest soil     

Mats G. Öquist  Kevin Petrone  Leif Klemedtsson 《Soil biology & biochemistry》2007,39(7):1809-1811

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.  相似文献   

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

Xuejun J. Liu  Arvin R. Mosier  Curtis A. Reule 《Soil biology & biochemistry》2007,39(9):2362-2370

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.  相似文献   

菜心的土壤钙、镁营养诊断指标及施肥效应研究   总被引：5，自引：0，他引：5  

陈琼贤  徐润生  吕业成  万云巧  郑少玲  曹健 《土壤通报》2008,39(1):110-113

在不同地方,不同钙、镁含量水平的菜园土壤进行菜心钙、镁肥田间试验。根据20个试验点的钙肥试验和15个试验点的镁肥试验结果,分别建立菜心相对产量与土壤交换性钙、镁含量的回归方程。研究结果表明:菜心产量与土壤交换性钙、镁含量分别呈抛物线相关;在质地为中壤土的菜田上种植菜心,土壤交换性钙的适宜含量为4.26￣9.60cmolL-1,交换性镁的适宜含量为2.01￣2.31cmolL-1;在参试的所有菜田中,施钙肥增产显著的菜田占50%,增产率为0.65￣33.8%;施镁肥增产显著的菜田占47%,增产率为-1.6%￣34.7%。  相似文献   

一氧化氮延缓草莓成熟衰老的生理效应   总被引：19，自引：4，他引：19  

朱树华  周杰  束怀瑞  王玲玲 《中国农业科学》2005,38(7):1418-1424

 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。  相似文献   

外源NO缓解果树胁迫的作用机理和研究进展     

陈志友 《中国果业信息》2013,42(2)

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。  相似文献   

嗜酸小球菌对凡纳滨对虾体液免疫因子的影响   总被引：3，自引：0，他引：3  

余德光  朱红友  王广军  谢骏  于方兆  黄志斌 《海洋水产研究》2006,27(5):51-55

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。  相似文献