通过不同的试验设计,3年间对风沙土进行秸秆等有机物料培肥,研究其结合态腐殖质中胡敏酸含量与E4/E6的变化,结果表明,不同有机物料培肥均能提高风沙土腐殖质中胡敏酸的含量,根据2000年测定结果,与CK相比,提高幅度在0.02～0.17 C g/kg之...通过不同的试验设计,3年间对风沙土进行秸秆等有机物料培肥,研究其结合态腐殖质中胡敏酸含量与E4/E6的变化,结果表明,不同有机物料培肥均能提高风沙土腐殖质中胡敏酸的含量,根据2000年测定结果,与CK相比,提高幅度在0.02～0.17 C g/kg之间,但胡敏酸与腐殖质的比值,随着培肥年限的增加,与CK处理比较,有降低的趋势,降低幅度在0.17％～2.23％之间。胡敏酸的E4/E6在有机物料处理间变化规律不明显,但其值都大于CK,随培肥年限的增加,处于动态的变化。展开更多
The changes in humic substances （HS） is fundamental in detecting soil carbon sequestration mechanisms in natural and cultivated environments. Based on a long-term trial, the amounts of water dissolved substances （...The changes in humic substances （HS） is fundamental in detecting soil carbon sequestration mechanisms in natural and cultivated environments. Based on a long-term trial, the amounts of water dissolved substances （WSS）, humic acid （HA）, fulvic acid （FA） and humin （HU） were determined to explore the impact of long-term fertilization on HS. Increases in the amounts of WSS, HA, FA and HU were significant different among the treatments with manure. A significant correlation was found between the increased soil organic carbon （SOC） and HS （R^2=0.98, P〈0.01）. The change in the E4/E6 ratio was significantly correlated with the increased SOC （R2=0.88, P〈0.01）, HA （R^2=0.91, P〈0.01）, FA （R^2=0.91, P〈0.01） and HU （R^2=0.88, P〈0.01）. The cluster was mainly divided into two parts as manure fertilization and inorganic fertilization, based on the increases in HA, FA and HU. These results suggest that long term fertilization with manure favours carbon sequestration in HS and is mainly stabilized as HU, while the HA becomes more aliphatic. We conclude that increases in SOC can be linked to changes in the molecular characteristics of HS fractions under long term fertilization.展开更多
Nitric humic acid was prepared by catalytic oxidation between nitric acid and Guizhou coal, with added catalysts. We investigated catalytic oxidation processes and the factors that affect the reactions. The effects of...Nitric humic acid was prepared by catalytic oxidation between nitric acid and Guizhou coal, with added catalysts. We investigated catalytic oxidation processes and the factors that affect the reactions. The effects of different catalysts, including NiSO4 support on active carbon （AC-NiS04）, NiS04 support on sil- icon dioxide （SiO2-NiSO4）, composites of SO42-1Fe203, Zr-iron and vanadium-iron composite were stud- ied. As well, we investigated nitric humic acid yields and the chemical structure of products by element analysis, FT-IR and E4/E6 （an absorbance ratio at wavelengths of 465 and 665 nm of humic acid alkaline extraction solutions）. The results show that the catalytic oxidation reaction with added catalysts can increase humic acid yields by 18.7%, 16.36% 12.94%, 5.61% and 8.59%, respectively. The highest yield of humic acid, i.e., 36.0%, was obtained with AC-NiSO4 as the catalyst. The amounts of C and H decreased with the amount of nitrogen. The increase in the E4/E6 ratio in catalytic oxidation of （Guizhou） coal shows that small molecular weights and high yields of nitric humic acid can be obtained by catalytic oxidation reactions.展开更多
神农架大九湖泥炭沼泽是中纬度亚热带地区的高山泥炭沼泽,其连续沉积的泥炭剖面蕴含了丰富的气候变化信息,对揭示我国中纬度地区不同时间尺度的气候环境变化有着重要意义。使用碱提取溶液吸光度法对大九湖泥炭吸光度进行测定,以E4/E6比...神农架大九湖泥炭沼泽是中纬度亚热带地区的高山泥炭沼泽,其连续沉积的泥炭剖面蕴含了丰富的气候变化信息,对揭示我国中纬度地区不同时间尺度的气候环境变化有着重要意义。使用碱提取溶液吸光度法对大九湖泥炭吸光度进行测定,以E4/E6比值表征腐殖化度,同时测定了泥炭的磁化率,通过AMS14C测年技术建立了神农架大九湖泥炭地的年代序列,结合区域的其他气候代用指标,分析大九湖泥炭磁化率与腐殖化度E4/E6的古气候意义:大九湖泥炭频率磁化率值高指示气候冷干,降水量小;磁化率值偏低指示气候暖湿,降水量大。E4/E6值高,腐殖化度低,指示气候冷干;值低,腐殖化度高,指示气候暖湿。探讨大九湖地区末次冰消期以来的气候变化,重建该区18.7 Ka BP的气候演化过程:末次冰期结束期(18.7~11.7 Ka BP)气候比较冷干,期间存在气候冷暖干湿交替波动;全新世(11.7~0 Ka BP)以来,气温开始回升,气候比较暖湿,期间也存在突发性降温事件,其中,全新世早期(11.7~9.3 Ka BP)气候冷暖干湿交替波动,总体冷湿;全新世中期(9.3~3.5 Ka BP)气候暖湿;全新世晚期(3.5~0 Ka BP)气候温干。展开更多
文摘通过不同的试验设计,3年间对风沙土进行秸秆等有机物料培肥,研究其结合态腐殖质中胡敏酸含量与E4/E6的变化,结果表明,不同有机物料培肥均能提高风沙土腐殖质中胡敏酸的含量,根据2000年测定结果,与CK相比,提高幅度在0.02～0.17 C g/kg之间,但胡敏酸与腐殖质的比值,随着培肥年限的增加,与CK处理比较,有降低的趋势,降低幅度在0.17％～2.23％之间。胡敏酸的E4/E6在有机物料处理间变化规律不明显,但其值都大于CK,随培肥年限的增加,处于动态的变化。
基金supported by the National Natural Science Foundation of China (30873470)the National Special Research Fund for Non-Profit Sector (Agriculture) (201203030)the grant from Qingdao Agricultural University, China (631214)
文摘The changes in humic substances （HS） is fundamental in detecting soil carbon sequestration mechanisms in natural and cultivated environments. Based on a long-term trial, the amounts of water dissolved substances （WSS）, humic acid （HA）, fulvic acid （FA） and humin （HU） were determined to explore the impact of long-term fertilization on HS. Increases in the amounts of WSS, HA, FA and HU were significant different among the treatments with manure. A significant correlation was found between the increased soil organic carbon （SOC） and HS （R^2=0.98, P〈0.01）. The change in the E4/E6 ratio was significantly correlated with the increased SOC （R2=0.88, P〈0.01）, HA （R^2=0.91, P〈0.01）, FA （R^2=0.91, P〈0.01） and HU （R^2=0.88, P〈0.01）. The cluster was mainly divided into two parts as manure fertilization and inorganic fertilization, based on the increases in HA, FA and HU. These results suggest that long term fertilization with manure favours carbon sequestration in HS and is mainly stabilized as HU, while the HA becomes more aliphatic. We conclude that increases in SOC can be linked to changes in the molecular characteristics of HS fractions under long term fertilization.
基金sponsored by the Shaanxi Key Scientific and Technological Project, China (No. 2010K07-20)the National Science and Technology Major Project (No. 2011ZX05037-003)
文摘Nitric humic acid was prepared by catalytic oxidation between nitric acid and Guizhou coal, with added catalysts. We investigated catalytic oxidation processes and the factors that affect the reactions. The effects of different catalysts, including NiSO4 support on active carbon （AC-NiS04）, NiS04 support on sil- icon dioxide （SiO2-NiSO4）, composites of SO42-1Fe203, Zr-iron and vanadium-iron composite were stud- ied. As well, we investigated nitric humic acid yields and the chemical structure of products by element analysis, FT-IR and E4/E6 （an absorbance ratio at wavelengths of 465 and 665 nm of humic acid alkaline extraction solutions）. The results show that the catalytic oxidation reaction with added catalysts can increase humic acid yields by 18.7%, 16.36% 12.94%, 5.61% and 8.59%, respectively. The highest yield of humic acid, i.e., 36.0%, was obtained with AC-NiSO4 as the catalyst. The amounts of C and H decreased with the amount of nitrogen. The increase in the E4/E6 ratio in catalytic oxidation of （Guizhou） coal shows that small molecular weights and high yields of nitric humic acid can be obtained by catalytic oxidation reactions.
文摘神农架大九湖泥炭沼泽是中纬度亚热带地区的高山泥炭沼泽,其连续沉积的泥炭剖面蕴含了丰富的气候变化信息,对揭示我国中纬度地区不同时间尺度的气候环境变化有着重要意义。使用碱提取溶液吸光度法对大九湖泥炭吸光度进行测定,以E4/E6比值表征腐殖化度,同时测定了泥炭的磁化率,通过AMS14C测年技术建立了神农架大九湖泥炭地的年代序列,结合区域的其他气候代用指标,分析大九湖泥炭磁化率与腐殖化度E4/E6的古气候意义:大九湖泥炭频率磁化率值高指示气候冷干,降水量小;磁化率值偏低指示气候暖湿,降水量大。E4/E6值高,腐殖化度低,指示气候冷干;值低,腐殖化度高,指示气候暖湿。探讨大九湖地区末次冰消期以来的气候变化,重建该区18.7 Ka BP的气候演化过程:末次冰期结束期(18.7~11.7 Ka BP)气候比较冷干,期间存在气候冷暖干湿交替波动;全新世(11.7~0 Ka BP)以来,气温开始回升,气候比较暖湿,期间也存在突发性降温事件,其中,全新世早期(11.7~9.3 Ka BP)气候冷暖干湿交替波动,总体冷湿;全新世中期(9.3~3.5 Ka BP)气候暖湿;全新世晚期(3.5~0 Ka BP)气候温干。
