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Calcium-bound and iron-and aluminium-bound humus extracted from different soils collected from north to south of China were characterized by chemical and spectroscopic methods.Meaningful differences in the composition and structure between them were revealed by ^13 C NMR,visible spectroscopy and elemental analysis.Results showed that the contents of carbon,hydrogen and nitrogen were higher in iron-and aluminium-bound humus than in calcium-bound humus while oxygen content in calcium-bound humus was shown to be higher .The calcium-bound humus had higher C/N and O/C ratios than iron-and aluminiumbound humus.The calcium-bound humic acid(HA1) showed higher E4/E6 ratios than iron-and aluminumboud,humic acid(HA2)while iron-and aluminum-bound fulvic acid(FA2) showed higher E4/E6 ratios than calcium-bound fulvic acid(FA1).An inverse relationship between E4/E6 ratios and aromaticity as determined by 13C NMR spectra was observerd for HA and FA from black soil.The 13C NMR spectroscopy revealed that HA2 was more aromatic than HA1.On the other ,FA1 exhibited a higher aromaticity than FA2. 相似文献
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不同温度制备的生物质炭对土壤有机碳矿化及腐殖质组成的影响 总被引:9,自引:6,他引:3
在150~600℃范围内制备生物质炭,并通过室内培养实验研究了施加不同温度制备的生物质炭对土壤有机碳矿化及腐殖质组成的影响。结果表明,随热解温度升高,生物质炭比表面积加大,芳香化结构加深。土壤中添加不同温度制备的生物质炭培养400d后,土壤有机碳的含量都有不同程度的增加。土壤有机碳的累积矿化量随热解温度升高而降低,且添加高温(≥400℃)制备生物质炭的土壤CO2累积释放量低于未添加生物质炭的土壤处理;添加低温(<400℃)制备生物质炭增加了土壤腐植酸和胡敏酸含量,而添加高温(≥400℃)制备生物质炭的土壤其腐植酸和胡敏酸含量的变化不显著。另外,添加生物质炭后,土壤H/F皆未发生显著变化,而胡敏酸的E4/E6值则在添加200℃和250℃制备的生物质炭时显著高于其他处理,添加500℃和600℃制备的生物质炭时显著低于其他处理。 相似文献
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黄瓜为喜温喜湿植物,生育适温为18~32℃,适宜的空气相对湿度为70?%,土壤湿度为85%~90%.黄瓜根系浅,应选择富含有机质、透气性好的腐植质壤土栽培,土壤应为弱酸性到弱碱性.雌花在蔓上着生的节位,早熟品种在第一至第三叶,晚熟品种在第十片叶附近.开花后8~18天,果实可达商品成熟.苗期无机营养的比例对黄瓜的性别分化有显著的影响,氮素用多时,雌花分化也多. 相似文献
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为验证"华绿"腐植质水溶性肥料在蔬菜生产中的应用效果,为大面积推广提供科学依据,2011年在番茄上进行了其肥效试验。结果表明,于番茄不同生育期喷施"华绿"腐植质水溶性肥料3次,植株茎粗增加15.08%,有效绿叶数增加2张,单株结果数增加3.5个,单株果重增加0.56kg,增产率达10.22%。 相似文献
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腐植酸钾对黄冠梨土壤肥力的影响 总被引:3,自引:1,他引:2
研究腐植酸钾对黄冠梨土壤中腐植质、氮、磷、钾含量的影响.结果表明:腐植酸钾显著提高土壤腐植质含量和速效氮、磷、钾含量,对土壤中全量养分影响不大.腐植酸钾具有改良土壤,增加肥效作用. 相似文献
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土壤水分状况对14C标记秸秆的腐解及腐殖质中碳素分布的影响 总被引:2,自引:0,他引:2
14C-tracer technique and closed incubation method were used to study straw 14C decomposition and distribution in different fractions of newly formed humus under different moisture regimes. Decomposition of straw 14C was faster during the initial days, and slower thereafter. Decay rate constants of straw 14C varied from 3.29 × 10-3 d-1 to 7.06 × 10-3 d-1. After 112 d incubation, the amount of straw 14C mineralized was 1.17~1.46 times greater in submerged soils than in upland soils. Of the soil residual 14C, 9.08%~15.73% was present in humic acid (HA) and 31.01%~37.62% in fulvic acid (FA). Submerged condition favored the formation of HA, and HA/FA ratio of newly formed humus (labelled) was greater in submerged soils than in upland soils. Clay minerals affected the distribution of straw 14C in different humus fractions. Proportion of 14C present in HA to 14C remaining in soil was greater in Vertisol than in Ultisol. 相似文献