Poorly crystalline iron and aluminium oxides contribute to the carbon saturation and sorption of dissolved organic carbon in the soil

Soil carbon (C) saturation implies an upper limit to a soil's capacity to store C depending on the contents of silt + clay and poorly crystalline Fe and Al oxides. We hypothesized that the poorly crystalline Fe and Al oxides in silt + clay fraction increased the C saturation and thus reduced the capacity of the soil to sorb additional C input. To test the hypothesis, we studied the sorption of dissolved organic carbon (DOC) on silt + clay fractions (<53 µm) of highly weathered oxic soils, collected from three different land uses (i.e., improved pasture, cropping and forest). Soils with high carbon saturation desorbed 38% more C than soils with low C saturation upon addition of DOC, whereas adsorption of DOC was only observed at higher concentration (>15 g kg^?1). While high Al oxide concentration significantly increased both the saturation and desorption of DOC, the high Fe oxide concentration significantly increased the desorption of DOC, supporting the proposition that both oxides have influence on the DOC sorption in soil. Our findings provide a new insight into the chemical control of stabilization and destabilization of DOC in soil.     

氮吸附法分析生物质焦孔隙结构

采用氮吸附法对4种生物质焦(稻壳、树叶、玉米秆、棉花秆)的孔隙结构进行测量,结果表明,不同种类焦样的比表面积和孔径分布有明显差别,树叶的比表面积最大,为242.21 m2·g-1,玉米秆的比表面积最小,为0.81 m2·g-1.850℃时,稻壳、树叶、玉米秆焦样的孔径分布曲线在微孔和中孔范围各有一个分布峰,而棉花秆焦样的孔径分布曲线只在中孔范围内出现一个分布峰.热解温度是影响孔隙结构的一个重要因素,在高温条件下,同步热解得到的焦样的比表面积较大,微孔较多.在本研究中,600℃、850℃的稻壳焦样和850℃的树叶焦样具有较大的比表面积,比较适合做吸附剂.     

Influence of the physical and chemical properties of soil on the retention process of isoxaflutole and its two main derivatives

Isoxaflutole is a new pre‐emergence herbicide for use in maize and sugarcane. Its two main derivatives are a diketonitrile derivative, the 2‐cyano‐3‐cyclopropyl‐1‐(2‐methanesulfonyl‐4‐trifluoromethylphenyl)propan‐1,3‐dione, named DKN, and a benzoic acid derivative, the 2‐methanesulfonyl‐4‐trifluoromethylbenzoic acid, named BA. The adsorption/desorption processes have never been studied for isoxaflutole (IFT) at high concentrations nor for BA, and the present work aimed at completing the knowledge of the behaviour of these three molecules in conditions close to those encountered in the context of agricultural use. The adsorption/desorption study was conducted on seven soils of different physical and chemical properties, using the batch equilibrium technique. During the experiments, IFT was chemically converted into DKN in a continuous manner. This reaction appeared to be dependent on the pH of the soil and was taken into account in the calculations of the adsorbed and desorbed amounts. The adsorption isotherms obtained were predominantly C‐shaped for IFT and DKN and S‐shaped for BA, but some differences appeared on a few soils. They fitted well the Freundlich equation, and the values of the Freundlich coefficient K_fa showed that, whatever the soil, IFT was more adsorbed than its two derivatives. The main parameter influencing the adsorption of IFT appeared to be the organic matter content, whereas this effect was not evident for DKN and BA. No correlation was found between the extent of adsorption and either clay content or pH of the soil, for the three molecules.     

差异显示法研究不同锌源对组织基因表达的影响

选用Avine肉用仔鸡作为试验对象 ,饲喂硫酸锌和蛋氨酸锌 2种锌源。采用银染差异显示技术进行差异基因的初步筛选。结果成功回收扩增差异条带 2 6条 ;其中加锌组 (硫酸锌组和蛋氨酸锌组 ) 2 3条 ,3条为缺锌组所特有。在加锌组的 2 3条中 ,6条为蛋氨酸锌组所特有 ,1 3条为硫酸锌组所特有 ,其余 4条为 2组所共有。这些初步筛选得到的差异基因尚需进一步进行克隆、测序和杂交进行验证。     

不同锌源对断奶小鼠生长及机体抗氧化能力的影响

选用断奶小鼠72只作为研究对象,随机分为3组(对照组,硫酸锌组和蛋氨酸锌组),每组设4个重复。测定体重、组织锌含量及相关生理生化指标,以研究硫酸锌、蛋氨酸锌2种不同锌供给形式对机体的生长效应及抗氧化能力的影响。结果表明,硫酸锌组和蛋氨酸锌组均能不同程度地提高小鼠体重,蛋氨酸锌组小鼠体重显著高于对照组与硫酸锌组(P<0.05)。饲粮中添加硫酸锌可提高小鼠肝脏和血清中的锌含量(P>0.05);蛋氨酸锌组小鼠肝脏和血清锌含量高于对照组(P<0.05)及硫酸锌组(P>0.05)。2种锌源均显著提高碱性磷酸酶(AKP)、谷胱甘肽过氧化物酶(GSHPx)活性(P<0.05),不同锌源间无明显差异(P>0.05)。添加不同的锌源不同程度地提高总抗氧化能力(TAOC)、总SOD(TSOD)、铜锌超氧化物歧化酶(CuZnSOD)活性(P<0.05),蛋氨酸锌组TAOC、TSOD显著高于硫酸锌组(P<0.05)。添加锌显著降低NO含量(P<0.05),蛋氨酸锌效果显著强于硫酸锌(P<0.05);一氧化氮合酶(NOS)活性表现出与NO相反的趋势(P>0.05)。     

P10B抗菌肽和硫酸小檗碱对肉鸡源大肠杆菌的体外联合抗菌作用研究

为了解P10B抗菌肽与硫酸小檗碱联合抗菌作用,进行P10B抗菌肽与硫酸小檗碱联用的体外抑菌试验。试验菌株为20株肉鸡源大肠杆菌菌株。采用微量肉汤稀释法测定P10B与硫酸小檗碱对大肠杆菌的最低抑菌浓度;棋盘稀释法测定两个药的分级抑菌浓度指数,判断联合抗菌效果。结果表明,在联合药敏试验中,两药呈协同作用的占10%,呈相加作用的占85%,呈无关作用的占5%。平均分级抑菌浓度指数为0.825,两种药联和用药效应主要表现为累加作用。     

Biochar Mitigates Salinity Stress in Potato

A pot experiment was conducted in a climate‐controlled greenhouse to investigate the growth, physiology and yield of potato in response to salinity stress under biochar amendment. It was hypothesized that addition of biochar may improve plant growth and yield by mitigating the negative effect of salinity through its high sorption ability. From tuber bulking to harvesting, the plants were exposed to three saline irrigations, that is 0, 25 and 50 mm NaCl solutions, respectively, and two levels of biochar (0 % and 5 % W/W) treatments. An adsorption study was also conducted to study the Na⁺ adsorption capability of biochar. Results indicated that biochar was capable to ameliorate salinity stress by adsorbing Na⁺. Increasing salinity level resulted in significant reductions of shoot biomass, root length and volume, tuber yield, photosynthetic rate (A_n), stomatal conductance (g_s), midday leaf water potential, but increased abscisic acid (ABA) concentration in both leaf and xylem sap. At each salinity level, incorporation of biochar increased shoot biomass, root length and volume, tuber yield, A_n, g_s, midday leaf water potential, and decreased ABA concentration in the leaf and xylem sap as compared with the respective non‐biochar control. Decreased Na⁺, Na⁺/K⁺ ratio and increased K⁺ content in xylem with biochar amendment also indicated its ameliorative effects on potato plants in response to salinity stress. The results suggested that incorporation of biochar might be a promising approach for enhancing crop productivity in salt‐affected soils.     

More evidence that anaerobic oxidation of methane is prevalent in soils: Is it time to upgrade our biogeochemical models?

Estimating future fluxes of CH₄ between land and atmosphere requires well-conceived process-based biogeochemical models. Current models do not represent the anaerobic oxidation of methane (AOM) in land surface soils, in spite of increasing evidence that this process is widespread. Our objective was to determine whether AOM, or potential AOM, commonly occurs in 20 hydromorphic soils spanning a wide range of chemical properties. Bulk soil samples were collected under shallow water near the shoreline of 15 recently drained fish ponds in southern Bohemia (Czech Republic), as well as from below the water table at 3 peatland locations in northeast Scotland and 2 acid sulfate soils on the southern coast of Finland. Each soil slurry was incubated under both oxic and anoxic conditions, with or without the addition of alternative electron acceptors (SO₄²⁻ and NO₃⁻) or H₂PO₄⁻. Here, “oxic” and “anoxic” conditions refer to anoxic soil respectively incubated in a headspace containing air or argon. Using the isotope dilution method, we determined the gross production and oxidation rates of CH₄ after 2 days incubation under oxic headspace conditions, and after 2, 21 and 60 days incubation under anoxic conditions. Large differences in net CH₄ fluxes were observed between soil types and between incubation conditions. AOM was detected in each of the 20 bulk soil samples, which spanned >6 pH units and 2 orders of magnitude in organic C content. Significant positive relationships were found between AOM and gross CH₄ production rates under anoxic conditions, resulting in AOM rates that were sometimes higher than CH₄ oxidation rates under oxic headspace conditions. There was no relationship between net and gross CH₄ production rates, such that 2 soil types could display similar low net rates, yet conceal very large differences in gross rates. The effects of alternative electron acceptors on AOM were idiosyncratic and resulted in no net trend. We did find, however, a negative effect of SO₄²⁻ and H₂PO₄⁻ on gross CH₄ production rates under anoxic and oxic conditions respectively. Under oxic headspace conditions, CH₄ oxidation was related to soil organic C content. Taken collectively, our results suggest that AOM, or potential AOM, is prevalent over a wide range of soil types, that AOM may contribute substantially to CH₄ oxidation in soils, and that AOM in soils should be integrated to current process-based CH₄ cycling models.     

茉莉花茶加工技术与吸香机理研究现状

为了进一步综合地认识茉莉花茶窨制的工艺本质、完善茉莉花茶窨制技术,本文综述和分析了茉莉花茶加工技术及吸香机理的研究现状,并对后续研究进行了展望。     

硫酸铜对泥鳅精子活力的影响

以泥鳅精子为受试材料,应用计算机辅助精子分析系统,研究硫酸铜(0.1、1、10 mg/L)对泥鳅的精子活力的影响.结果表明,在0 h试验组,0.1 mg/L的硫酸铜明显降低泥鳅精子运动速度,1 mg/L的硫酸铜对运动时间和速度产生显著抑制作用,10 mg/L的硫酸铜时运动百分数、运动时间和速度都产生明显影响(P<0.0...