共查询到19条相似文献，搜索用时 375 毫秒
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川中丘陵区人工桤柏混交林根呼吸对土壤总呼吸的贡献 总被引：1，自引：0，他引：1
采用挖壕沟法和根系生物量外推法对桤柏混交林地根呼吸在土壤总呼吸的贡献进行了为期1 a的对比研究。研究表明,两种方法测得的根呼吸平均速率分别为0.64μmol CO2/（m^2.s）和0.54μmol CO2/（m^2.s）,挖壕沟法高于根系生物量外推法的测定结果。两种方法计算的根呼吸占土壤呼吸的比例具有明显的季节变化,均表现为夏季（5～6月）较高而冬季（1～2月）较低,变化范围分别为13%～51%、11%～56%,平均分别为34%和31%;林木生长季节根呼吸比例均高于非生长季,两种方法测定的林木生长季根呼吸比例分别为41%和38%。方差分析表明两种方法测定根呼吸比例之间差异不显著（p〉0.05）。 相似文献
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采用重量法测定了自制磷酸亚铁锂碳复合物中的碳含量,且将碳过滤分离后,制得了样品溶液,用来测定其中的元素含量。采用EDTA络合滴定法和邻菲啰啉分光光度法测得铁离子质量分数分别为33.88%、33.77%,测定的RSD分别为0.1%、0.6%。两种方法的测定结果很接近,但是通过F检验法得到EDTA络合滴定法的精密度显著高于邻菲啰啉分光光度法的精密度。采用磷钼酸喹啉重量法和磷钒钼黄光度法测得磷的质量分数分别为19.22%、19.36%,测定的RSD为1.81%、1.89%。两种方法的测定结果很接近,通过F检验法发现两种方法的精密度不存在显著性差异,通过t检验法发现两种方法在置信度为90%时,不存在显著性差异。 相似文献
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为了明确好氧反硝化微生物在氮元素污染湿地水体原位修复工程中的可行性,采用培养基富集,NO3-BTB平板划线法,从大庆湿地筛选到一株好氧反硝化细菌DQ1,通过生理生化测定和16S rRNA测定(登录号为:JQ669957)鉴定为恶臭假单胞菌(Pseudomonas putida)。菌株DQ1在以硝酸盐为唯一氮源,以柠檬酸为唯一碳源,在30℃的条件下静止培养30 h,总氮(TN)去除率达到91.9%,整个过程中没有检测到亚硝态氮(NO2-—N)的积累;在初始氮源浓度为1 930 mg/L,以柠檬酸、酒石酸钾钠、无水乙酸、葡萄糖和乙醇等为唯一碳源,5d总氮去除率分别为97.4%、97.1%、97.2%、97.6%和98.5%。当pH为6.5、6.95、7.45、8.0和8.5时,5 d总氮去除率分别为93.71%、97.27%、97.59%、97.35%和96.85%;当初始pH为7.45时,总氮去除率最高达97.59%,菌株DQ1在温度20~37℃范围内,5 d总氮去除率分别为98.03%、98.12%、98.23%和98.05%。 相似文献
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《盐湖研究》2002,(4)
ＴＰＤ软件绘制水盐体系三元相图夏树屏 ,陈世荣 ,王 波 ,李明华 ,高世扬 ( 1 .1 )……………论四川盆地三叠系盐类热融水溶变质对找钾方向的控制林耀庭 ,郑茂全 ( 1 .8)…………………腾格里沙漠地区盐湖钾盐资源特征李博昀 ,刘振敏 ,徐少康 ,刘国庆 ( 1 .1 8)…………………固体钾肥产品中钾含量的放射性测定祁永唐 ,王相明 ,李青凤 ,王庆忠 ( 1 .2 4)………………柴达木盆地中部盐湖环境遥感初步解译张 辉 ,韩凤清 ( 1 .2 8)…………………………………40℃时ＭｇＯ·2Ｂ2 Ｏ3-1 8%ＭｇＳＯ4-Ｈ2 Ｏ过饱和溶液结晶动力学研究马玉涛 ,夏… 相似文献
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紫色土的钾素形态转化 总被引：1，自引：0，他引：1
采用室内盆钵培养方法 ,研究侏罗纪蓬莱镇组 (J3P)、沙溪庙组 (J2 S)、遂宁组 (J3S)和白垩纪城墙岩群 (K1 C)紫色岩层发育土壤的钾素形态转化。结果表明 ,一年后 ,紫色土交换性钾增加 2 0mg.kg- 1 以上 ,非交换性钾增加 10 .5 8mg .kg- 1 ,结构钾减少了 31.5 6mg .kg- 1 。交换性钾、非交换性钾增加顺序分别为 :J3P >J3S >J2 S >K1 C及K1 C >J3P >J2 S >J3S ;结构钾降低的顺序为 :J3P >J3S >K1 C >J2 S。紫色土交换性钾、非交换性钾及结构钾互为消长有利于土壤源源不断地供给作物有效态钾素 ,一定程度弥补因作物带走的钾。 相似文献
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柴达木盆地是我国重要的钾肥基地,年产氯化钾超过700×10~4t,副产尾盐超过1 000×10~4t,尾盐的主要组分是氯化钠,并夹带少量的氯化钾。通过精制试验研究,进一步回收氯化钾,氯化钠则作为纯碱原料,实现了尾盐的梯级综合利用,对促进盐湖循环经济发展具有重要意义。试验表明,采用二段洗涤工艺,结合喷淋和搅拌两种洗涤方式处理钾肥生产浮选尾盐,浮选尾盐经二段洗涤所得产品中氯化钠含量达到92.54%,符合纯碱所需原盐指标要求;母液中的氯化钾富集到一定程度后,回收可作为钾肥生产原料。 相似文献
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J. E. Sherwood M. J. Kokkinn W. D. Williams 《International Journal of Salt Lake Research》1994,3(2):159-173
Standard methods for the determination of phosphorus as phosphate ion are now well established for fresh and marine waters. In highly saline waters, however, salt effects due to ionic strength, or to particular ions present, may result in method interferences. Three methods of analysis of phosphate based on the formation of phosphomolybdenum blue complexes have been evaluated here for hypersaline waters. Stannous chloride reduction in aqueous media exhibits a substantial salt effect and its use is not recommended. Stannous chloride reduction following extraction into non aqueous solvents shows a significant salt effect (up to 30 per cent) in solutions of salinity >100 g L–1. Dilution of hypersaline waters to below this salinity may overcome the salt effect but the method suffers from other disadvantages involving resource constraints and health and safety considerations. Ascorbic acid reduction, catalysed by antimony (III) ions, appears to offer the most promise for hypersaline waters. Turbidity in samples having high salinity (> 100 g L–1) and high phosphorus concentrations (> 500 g P L–1) changes the spectral characteristics of solutions but linear calibration curves still result for concentrations in the range 400 to 1,000 g P L–1. The occurrence of turbidity is also affected by the ionic composition of hypersaline waters since solutions made from sea salt give different results to those made from sodium chloride. Dilution of samples, to give salinities less than 100 g L–1 prior to reduction is recommended to avoid turbidity. The salt effect in these lower salinity waters is less than 3 per cent up to 100 g L–1. 相似文献
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Research for changes of soil water and salt is an important content of land sciences and agriculture sciences in arid and semi arid regions. In this paper, sampling in actual agricultural fields, laboratory analysis of soil samples and statistical analysis methods are used to quantitatively analyze soil salinity changes under different irrigation methods throughout the cotton growing season in Shihezi reclamation area. The results show that irrigation methods play an important role in soil salt content in the surface soil (0-20 cm) and sub-deep soil (40-60 cm), followed by deep soil layer (60-100 cm) and root soil layer (20-40 cm). Furrow irrigation yields the maximum soil salt content in deep layer (60-100 cm) or sub-deep layer (40-60 cm) and the maximum salinity occurs in the first half of the cotton growing season (June or earlier). In contrast, drip irrigation yields the maximum soil salinity in the root layer (20-40 cm) or sub-deep (40-60 cm), and this usually appears in the second half growing season (July or after). The ratio of chloride ion to sulfate ion (Cl-/SO42-) and its change in the soil are on the rise under furrow irrigation, while the value first increased and then decreased with a peak point in June under drip irrigation. This suggests that furrow irrigation may shift the type of soil salinization to chloride ion type moreso than drip irrigation. Potassium and sodium ion contents of the soil show that soil sodium+potassium content will drop after the first rise under furrow irrigation and the value is manifested by fluctuations under drip irrigation. Potassium+sodium content change is relatively more stable in the whole cotton growth period under irrigation methods. The maximum of sodium and potassium content of the soil usually occur in deep soil layer (60-100 cm) or sub-deep soil layer (40-60 cm) in most sample points under furrow irrigation while it is inconsistent in different sample points under drip irrigation. A nonparametric test for paired samples is used to analyze differences of soil salt content under different irrigation methods. This analysis shows that the impact of irrigation on soil salinity is most significant in July, followed by August, June, May, and April in most sample points. The most significant impact of irrigation methods occurs in the surface soil layer (0-20 cm), followed by deep layer (60-100 cm), root layer (20-40 cm) and sub-deep (40-60 cm). These conclusions will be benefitial for mitigation of soil salinization, irrigation and fertilization and sustainable land use. 相似文献
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