利用凝胶扩散法测定刺萼龙葵种子中β-甘露聚糖酶的活性

β-甘露聚糖酶是种子萌发过程中降解胚乳细胞壁的关键酶,明确其活性的动态变化可为揭示杂草种子的休眠萌发机制提供重要依据。以外来杂草刺萼龙葵Solanum rostratum Dunal种子为材料,建立了种子中β-甘露聚糖酶活性的检测方法—凝胶扩散法。利用凝胶扩散法对不同贮存时间及贮存条件下刺萼龙葵种子中β-甘露聚糖酶的活性进行了检测,发现贮存3年以上的种子中该酶的活性为0.03 nmol/(min·mg),显著低于贮存3年以下的种子中的酶活性0.15 nmol/(min·mg),而湿润冷藏的种子中β-甘露聚糖酶的活性为0.12 nmol/(min·mg),显著高于干燥冷藏的种子的酶活性0.02 nmol/(min·mg)。实际应用结果表明,凝胶扩散法综合了传统方法的优势,检测特异性强、灵敏度高、重复性好,可同时检测大量种子样品,具有良好的实用性。     

陆上输油管道溢油扩散规律及泄漏后果研究进展

输油管道一旦泄漏不但会造成直接经济损失,而且将对周围环境、沿线居民带来不利影响,掌握泄漏油品在周围环境中的渗流、地表扩散以及蒸发情况,对于开展管道应急处理和泄漏后果评价至关重要。结合陆上输油管道泄漏事故特点,从事故条件下的泄漏量、泄漏油品的流动扩散规律以及泄漏后果等方面入手,对成品油管道泄漏油品研究成果进行了归纳总结,同时为进一步研究泄漏油品在周围环境的扩散过程,预估泄漏后果并制定合理的应急处理方案提出了建议。     

牛角瓜根的抑菌活性研究

以牛角瓜根为实验材料,采用索氏提取法,以4种不同溶剂(石油醚、氯仿、乙酸乙酯、甲醇)对牛角瓜的根进行提取,并采用纸片琼脂扩散法对粗提物的抑菌活性进行了评价,供试菌包括白色念珠菌等6种真菌和金黄色葡萄球菌等7种细菌。结果表明:石油醚粗提物对枯草芽孢杆菌、白色念珠菌、黑曲霉菌、大肠埃希氏菌都表现出良好的抑菌活性,且抑菌效果接近或优于阳性对照氟康唑,对尖孢镰刀菌和鲍曼不动杆菌也表现出良好的抑菌活性;氯仿粗提物对白色念珠菌及粪链球菌表现出良好的抑菌活性;乙酸乙酯粗提物对粪链球菌表现出最好的抑菌活性;甲醇粗提物的抑菌活性较弱。     

生物炭对黑土区土壤水分扩散与溶质弥散持续效应研究

为探究施用生物炭对黑土区坡耕地土壤水分扩散和溶质弥散的持续效应，于2016—2019年在1.5°、3°、5°的径流小区开展了生物炭持续效应试验，分析了单次施加生物炭对土壤容重、孔隙度、有机质含量、Boltzmann变换参数ξ、非饱和土壤水分扩散率D(θ)、非饱和土壤水动力弥散系数Dsh(θ)的持续作用。结果表明：土壤中单次添加生物炭后的4年内均可显著降低土壤容重、提高土壤孔隙度、增加土壤中有机质含量，且各指标变化率均随坡度增大、施炭年限延长而减小；坡度、年份、是否施用生物炭3个因素中，对土壤容重、孔隙度、有机质含量影响程度最大的均为是否施用生物炭；施用生物炭增大了ξ，且ξ随坡度增加、施炭后年限延长逐年减小。2016—2019年D(θ)与Dsh(θ)均随土壤含水率的增加而迅速增加。当土壤含水率小于等于042cm3/cm3时，生物炭抑制土壤水分扩散；当土壤含水率大于0.42cm3/cm3时，生物炭促进土壤水分扩散。当土壤含水率小于等于0.36cm3/cm3时，生物炭抑制土壤中NaCl溶液的弥散；当土壤含水率大于0.36cm3/cm3时，生物炭可以促进土壤中NaCl溶液的弥散。试验区θ处于0.20~0.35cm3/cm3，故施用生物炭对水分扩散、NaCl溶液弥散均具有抑制效果，且生物炭对水分扩散和溶液弥散抑制效果均随坡度增加、施炭后年限延长而减弱。     

环境温度对LNG泄漏扩散影响的数值模拟

环境温度导致的气云密度差和大气湍流变化是LNG泄漏扩散的主要影响因素,研究环境温度变化对LNG扩散规律的影响尤为重要。采用Fluent软件中组分输运和Realizable k-ε湍流模型,建立LNG地面泄漏气云扩散数值模型,探究环境温度对LNG泄漏扩散过程中甲烷体积分数的分布规律、气云密度、大气湍流强度的影响。结果表明:当环境温度较低时,LNG气云中各甲烷体积分数线出现"锯齿状"现象,造成甲烷爆炸下限(Low Flammability Limit,LFL)、1/2 LFL的水平扩散范围均增大;当环境温度较高时,甲烷LFL最远扩散距离较低温环境多115 m,造成甲烷1/2 LFL的水平顺风方向扩散距离增大;甲烷体积分数大于1/2 LFL的区域的大气湍流强度增幅则随温度升高而增加,而甲烷体积分数小于1/2 LFL的区域的大气湍流强度增幅随温度的升高而减小;在泄漏源周围100~200 m内,由于"逆温"所造成的大气湍流强度的增幅达0.79倍。研究结果可为LNG泄漏危害区域预测、安全储运、应急救援提供参考。     

Assessment of diffusive phosphate supply in soils by microdialysis

Standard procedures to assess P availability in soils are based on batch experiments with various extractants. However, in most soils P nutrition is less limited by bulk stocks but by strong adsorption and transport limitation. The basic principle of root‐phosphate uptake is to strip phosphate locally from the solid phase by forming a radial depletion zone in the soil solution, optionally enhanced by release of mobilizing substances. Microdialysis (MD), a well‐established method in pharmacokinetics, is capable to mimic important characteristics of P root uptake. The sampling is by diffusional exchange through a semipermeable membrane covering the probes with their sub‐mm tubular structure. Additionally, the direct environment of the probe can be chemically modified by adding, e.g ., carboxylates to the perfusate. This study is the first approach to test the applicability of MD in assessing plant available phosphate in soils and to develop a framework for its appropriate use.We used MD in stirred solutions to quantify the effect of pumping rate, concomitant ions, and pH value on phosphate recovery. Furthermore, we measured phosphate yield of top‐soil material from a beech forest, a non‐fertilized grassland, and from a fertilized corn field. Three perfusates have been used based on a 1 mM KNO₃ solution: pure (1), with 0.1 mM citric acid (2), and with 1 mM citric acid (3). Additionally, a radial diffusion model has been parametrized for the stirred solutions and the beech forest soil.Results from the tests in stirred solutions were in good agreement with reported observations obtained for other ionic species. This shows the principal suitability of the experimental setup for phosphate tests. We observed a significant dependency of phosphate uptake into the MD probes on dialysate pumping rate and on ionic strength of the outside solution. In the soils, we observed uptake rates of the probes between 1.5 × 10⁻¹⁵ and 6.7 × 10⁻¹⁴ mol s⁻¹ cm⁻¹ in case of no citrate addition. Surprisingly, median uptake rates were mostly independent of the bulk soil stocks, but the P‐fertilized soil revealed a strong tailing towards higher values. This indicates the occurrence of hot P spots in soils. Citrate addition increased P yields only in the higher concentration but not in the forest soil. The order of magnitude of MD uptake rates from the soil samples matched root‐length related uptake rates from other studies. The micro‐radial citrate release in MD reflects the processes controlling phosphate mobilization in the rhizosphere better than measurements based on “flooding” of soil samples with citric acid in batch experiments. Important challenges in MD with phosphate are small volumes of dialysate with extremely low concentrations and a high variability of results due to soil heterogeneity and between‐probe variability. We conclude that MD is a promising tool to complement existing P‐analytical procedures, especially when spatial aspects or the release of mobilizing substances are in focus.     

不同立地类型根灌、滴灌水分扩散规律

为掌握根灌、滴灌在不同立地类型土壤中的水分扩散规律,通过不同灌水梯度试验,采用挖剖面和直观观测法,研究了根灌和滴灌在不同立地类型土壤水分的垂直和水平扩散规律。结果表明:风沙土中根灌、滴灌水分垂直扩散明显小于水平扩散,且灌水时间与扩散速率均呈负相关对数关系。沙质壤土中根灌水分垂直扩散明显小于水平扩散,滴灌则垂直扩散速率大于水平扩散,两者差异不明显;灌水时间与扩散速率呈负相关对数关系。灰棕漠土中根灌初期水分垂直扩散和水平扩散相同,随时间增大,水平扩散速率大于垂直扩散;滴灌则垂直扩散速率大于水平扩散,但两者差异不明显;灌水时间与扩散速率也呈负相关对数关系。总体来看,根灌在不同立地类型土壤中的水分无论垂直扩散速率还是水平扩散速率都表现为:沙质壤土风沙土灰棕漠土;滴灌则无论水平扩散速率还是垂直扩散速率都表现为:灰棕漠土风沙土沙质壤土,两者扩散规律明显不同。