Controls on suppression of methane flux from a peat bog subjected to simulated acid rain sulfate deposition

The effect of acid rain SO42− deposition on peatland CH4 emissions was examined by manipulating SO42− inputs to a pristine raised peat bog in northern Scotland. Weekly pulses of dissolved Na2SO4 were applied to the bog over two years in doses of 25, 50, and 100 kg S ha−1 yr−1, reflecting the range of pollutant S deposition loads experienced in acid rain-impacted regions of the world. CH4 fluxes were measured at regular intervals using a static chamber/gas chromatographic flame ionization detector method. Total emissions of CH4 were reduced by between 21 and 42% relative to controls, although no significant differences were observed between treatments. Estimated total annual fluxes during the second year of the experiment were 16.6 g m−2 from the controls and (in order of increasing SO42− dose size) 10.7, 13.2, and 9.8 g m−2 from the three SO42− treatments, respectively. The relative extent of CH4 flux suppression varied with changes in both peat temperature and peat water table with the largest suppression during cool periods and episodes of falling water table. Our findings suggest that low doses of SO42− at deposition rates commonly experienced in areas impacted by acid rain, may significantly affect CH4 emissions from wetlands in affected areas. We propose that SO42− from acid rain can stimulate sulfate-reducing bacteria into a population capable of outcompeting methanogens for substrates. We further propose that this microbially mediated interaction may have a significant current and future effect on the contribution of northern peatlands to the global methane budget.

辽宁丹东地区柞树菌根真菌生态分布的研究

通过 5年连续调查研究 ,发现辽宁丹东地区天然次生柞林中及部分柞树经济林中柞树菌根菌种类共有 36种 ,隶属于 7个科 13个属 .在此基础上研究分析了柞树菌根菌的生态分布与共生树种、树龄及季节的关系 .结果表明 ,与蒙古栎共生的菌根菌种类最多 ,达 2 9种 ;红菇属种类与柞树共生的树龄范围最广 ,鹅膏属种类偏重于与树龄较大的柞树共生 ;夏季的 7、8月份为菌根菌发生的高峰期 ,75 %的种类在 7月份发生 ,10 0 %的种类在 8月份发生 .8月中下旬菌根菌发生的相对密度最高 ,分别为 19.5 %和 18.4 % .

不同倍性小麦材料对水分和密度条件的响应

以栽培一粒(2n)、栽培二粒(4n)和长武134(6n)为材料在大型活动防雨棚条件下研究不同倍性小麦材料在不同密度和水分条件下的产量适应性变化。结果发现,在两种水分条件下随着染色体倍性从2n→6n的增加,产量、千粒重、水分利用效率(WUE)和收获指数均呈增加趋势,在水分胁迫下各材料穗粒数和穗数则呈降低趋势,而在正常供水下穗粒数则呈增加趋势。在水分胁迫下栽培一粒、栽培二粒和长武134最高产量分别出现在中、低、高密度群体,而同一材料不同密度群体间变异系数分别为6.73%,1.98%,9.07%;不同倍性材料千粒重均随着密度增加而减小,而穗数则逐渐增加,二倍体的穗粒数以中密度最高,四倍体的穗粒数随着群体密度的增加而减小,六倍体则相反;三种材料WUE和收获指数分别以低、高、低密度最高。正常供水下随着染色体倍性从2n→6n的增加,三个倍性材料最高产量分别出现在高、低、低密度群体,而同一材料不同密度群体间变异系数分别为6.01%,17.12%,2.46%;千粒重表现为中密度>低密度>高密度,而穗粒数均以低密度群体最高,二倍体和四倍体以高密度群体最低,六倍体则以中密度群体最低,穗数则随着密度群体增加而增加;二倍体WUE以高...

CaCl_2对细颗粒泥沙静水絮凝沉降的影响

细颗粒泥沙的絮凝或分散对土壤渗透性、土壤可蚀性有重要作用 ,是水土保持研究的重要内容。在 Ca Cl2 浓度为 0～ 1.0 mmol/L ,泥沙浓度为 10 g/L时 ,用吸管法研究了 Ca Cl2 对细颗粒泥沙絮凝沉降的影响。结果表明 :泥沙沉降分 2个阶段 ,分选沉降段和絮凝沉降段 ;在絮凝沉降段 ,Ca Cl2 浓度越大 ,絮凝沉降越快。但较高浓度时 ,细颗粒泥沙平均沉速反而随 Ca Cl2浓度增大而逐渐减小 ;泥沙浓度随时间呈指数衰减 ;细颗粒泥沙絮凝临界粒径为 0 .0 3mm。

旱地冬小麦氮磷自然供给能力及其吸收氮磷来源的长期定位试验

利用在黄土旱塬上布置的 13年小麦连作肥料定位试验资料 ,研究了旱地冬小麦氮磷的自然供给能力和吸收来源于肥料和土壤的氮磷相对比例。结果表明 ,旱地冬小麦氮素的自然供给能力为 2 6 6 8～ 2 7 4 9kg/hm2 ,平均为 2 7 2kg/hm2 ;磷素自然供给能力为 5 2 1～ 8 4 9kg/hm2 ,平均为 7 31kg/hm2 。小麦吸收氮素有 51 9%～ 76 8%来自氮肥 ,平均为 6 6 6 % ;而来自土壤为2 3 2 %～ 4 8 1% ,平均 33 4 %。小麦吸收磷素来源于肥料的为 13 6 %～ 4 7 8% ,平均为2 8 7% ;来源于土壤为 52 2 %～ 86 4 % ,平均为 71 3%。同一肥底基础上 ,随肥料用量的增加 ,小麦吸收氮或磷素来源于肥料的比例也增大 ,而来源于土壤的比例逐渐减少。本试验条件下 ,氮肥利用率变幅为 32 6 %～ 6 6 0 % ,平均为 51 1% ;磷肥利用率变幅为 1 72 %～ 14 0 2 % ,平均为 7 0 %

沈阳市行道树树种的选择与配置

采取典型抽样的方法对沈阳市行道树进行了全面的群落调查。结果表明 ,研究区内行道树共 13科 ,2 4属 ,2 2 91株 ,森林覆盖率为 15 13%。胸径 <0 2 5m(1级胸径 )和 0 2 5～ 0 5m(2级胸径 )的树木分别占 4 3 0 %、17 9% ;树高 <4 6m (1级 )的树木占 4 9 8% ,介于 4 6～10 7m(2级 )为 4 3 3% ;健康状况为中等以上 ,沈阳市行道树处于种群稳定时期 ,但树种多样性指数不高 ,结构单一。根据城市的自然条件和行道树的选择标准 ,提出了沈阳市行道树树种选择与配置的对策与建议。

井冈山森林凋落物分解动态及磷、钾释放速率

应用网袋分解法对井冈山地区亚热带常绿阔叶林、针阔叶混交林和高山矮林地上和地下(10cm)2个分解组的叶凋落物进行了连续2年的分解试验,测定了凋落物的分解速率以及P、K元素的释放动态.结果表明:3种林分叶凋落物残留率与时间呈负指数衰减关系.各林分凋落物干质量损失前期较快,第1年末两组平均质量损失率分别为50.6%(常绿阔叶林)、41.7%(针阔叶混交林)和40.13%(高山矮林),且地上组显著高于地下组;后期较慢,至第2年末2组平均质量损失率分别达到60.95%(常绿阔叶林)、57.06%(针阔叶混交林)和

1.54 mu m near-infrared photoluminescent and electroluminescent properties of a new Erbium (111) organic complex

The crystal structure of Er(PM)(3)(TP)(2) [PM = 1-Phenyl-3-methyl-4-isobutyryl-5-pyrazoloiie, TP = triphenyl phosphine oxide] was reported and its photoluminescence properties were studied by UV-vis absorption, excited, and emission spectra. The Judd-ofelt theory was introduced to calculate the radiative transition rate and the radiative decay time of 3.65 ms for the I-4(13/2) -> I-4(15/2) transition of Er3+ ion in this complex.

Near-infrared luminescent properties and natural lifetime calculation of a novel Er3+ complex

in this communication, a novel Er3+ complex Er(PT)(3)TPPO [PT = 1-phenyl-3-methyl-4-tert-butylbenzoyl-5-pyrazolone, TPPO = triphenyl phosphine oxide] is successfully synthesized and characterized by elemental analysis and single-crystal X-ray diffraction. Its optical properties and the energy transfer process from the ligand PT to the Er3+ ion are investigated, the typical near-infrared (NIR) luminescence (centered at around 1530 nm) is attributed to the I-4(13/2) -> I-4(15/2) transition of Er3+ ion which results from the efficient energy transfer from PT to Er3+ ion (an antenna effect). The wider full width at half maximum (78 nm) peaked at 1530 nm in the emission spectrum and the Judd-Ofelt theory calculation on the radiative properties suggest that Er(PT)(3)TPPO should be a promising candidate for tunable lasers and planar optical amplifiers.

Host-sensitized luminescence of Dy3+, Pr3+, Tb3+ in polycrystalline SrIn2O4 for field emission displays

SrIn2O4:Dy3+/Pr3+/Tb3+ white/red/green phosphors were prepared by the Pechini sol-gel process. X-ray diffraction (XRD), field-emission scanning electron microscopy (FE-SEM), diffuse reflectance, photoluminescence, cathodoluminescence spectra, and lifetimes were utilized to characterize the samples. XRD reveal that the samples begin to crystallize at 800 degrees C and pure SrIn2O4 phase can be obtained at 900 degrees C. FE-SEM images indicate that the SrIn2O4:Dy3+, SrIn2O4:Pr3+, and SrIn2O4:Tb3+ samples consist of fine and spherical grains with size around 200-400 nm. Under the excitation of ultraviolet light and low-voltage electron beams (1 - 5 kV), the SrIn2O4:Dy3+, SrIn2O4: Pr3+, and SrIn2O4: Tb3+ phosphors show the characteristic emissions of Dy3+ (F-4(9/2) - H-6(15/2) at 492 nm and 4F(9/2) - 6H(13/2) at 581 nm, near white), Pr3+ (P-3(0) - H-3(4) at 493 nm, D-1(2) - H-3(4) at 606 nm, and P-3(0) - H-3(6) at 617 nm, red) and Tb3+ (D-5(4) - F-7(6,5,4,3) transitions dominated by D-5(4) - F-7(5) at 544 nm, green), respectively. All of the luminescence resulted from an efficient energy transfer from the SrIn2O4 host lattice to the doped Dy3+, Pr3+, and Tb3+ ions, and the luminescence mechanisms have been proposed.

Enhanced photoluminescence of Ba2GdNbO6: Eu3+/Dy3+ phosphors by Li+ doping

The Ba2GdNbO6: Eu3+/Dy3+ and Li+-doped Ba2GdNbO6: Eu3+/Dy3+ phosphors were prepared by solid-state reaction process. X-ray diffraction (XRD), field emission scanning electron microscopy (FE-SEM) and photoluminescence (PL) as well as lifetimes, was utilized to characterize the resulting phosphors. Under the excitation of ultraviolet light, the Ba2GdNbO6: Eu3+/Dy3+ and Li+-doped Ba2GdNbO6: Eu3+/Dy3+ show the characteristic emissions of Eu3+ (D-5(0)-F-7(1,2,3) transitions dominated by D-5(0)-F-7(1) at 593 nm) and Dy3+ (F-4(9/2)-H-6(15/2),(13/2) transitions dominated by F-4(9/2)-H-6(15/2) at 494 nm), respectively. The incorporation of Li+ ions into the Ba2GdNbO6: Eu3+/Dy3+ phosphors has enhanced the PL intensities depending on the doping concentration of Li+, and the highest emission was obtained in Ba2Gd0.9NbO6: 0.10Eu(3+), 0.01Li(+) and Ba2Gd0.95NbO6: 0.05Dy(3+), 0.07Li(+), respectively. An energy level diagram was proposed to explain the luminescence process in the phosphors.