The stable isotope signature of methane emitted from plant material under UV irradiation

Recent experiments have shown that dry and fresh leaves, other plant matter, as well as several structural plant components, emit methane upon irradiation with UV light. Here we present the source isotope signatures of the methane emitted from a range of dry natural plant leaves and structural compounds. UV-induced methane from organic matter is strongly depleted in both ¹³C and D compared to the bulk biomass. The isotopic content of plant methoxyl groups, which have been identified as important precursors of aerobic methane formation in plants, falls roughly halfway between the bulk and CH₄ isotopic composition. C3 and C4/CAM plants show the well-established isotope difference in bulk ¹³C content. Our results show that they also emit CH₄ with different δ¹³C value. Furthermore, δ¹³C of methoxyl groups in the plant material, and ester methoxyl groups only, show a similar difference between C3 and C4/CAM plants. The correlation between the δ¹³C of emitted CH₄ and methoxyl groups implies that methoxyl groups are not the only source substrate of CH₄.Interestingly, δD values of the emitted CH₄ are also found to be different for C3 and C4 plants, although there is no significant difference in the bulk material. Bulk δD analyses may be compromised by a large reservoir of exchangeable hydrogen, but no significant δD difference is found either for the methoxyl groups, which do not contain exchangeable hydrogen. The δD difference in CH₄ between C3 and C4 plants indicates that at least two different reservoirs are involved in CH₄ emission. One of them is the OCH₃ group, the other one must be significantly depleted, and contribute more to the emissions of C3 plants compared to C4 plants. In qualitative agreement with this hypothesis, CH₄ emission rates are higher for C3 plants than for C4 plants.     

Phosphorus recovery from biogas fermentation liquid by Ca–Mg loaded biochar

Shortage in phosphorus (P) resources and P wastewater pollution is considered as a serious problem worldwide. The application of modified biochar for P recovery from wastewater and reuse of recovered P as agricultural fertilizer is a preferred process. This work aims to develop a calcium and magnesium loaded biochar (Ca–Mg/biochar) application for P recovery from biogas fermentation liquid. The physico-chemical characterization, adsorption efficiency, adsorption selectivity, and postsorption availability of Ca-Mg/biochar were investigated. The synthesized Ca–Mg/biochar was rich in organic functional groups and in CaO and MgO nanoparticles. With the increase in synthesis temperature, the yield decreased, C content increased, H content decreased, N content remained the same basically, and BET surface area increased. The P adsorption of Ca–Mg/biochar could be accelerated by nano-CaO and nano-MgO particles and reached equilibrium after 360 min. The process was endothermic, spontaneous, and showed an increase in the disorder of the solid–liquid interface. Moreover, it could be fitted by the Freundlich model. The maximum P adsorption amounts were 294.22, 315.33, and 326.63 mg/g. The P adsorption selectivity of Ca–Mg/biochar could not be significantly influenced by the typical pH level of biogas fermentation liquid. The nano-CaO and nano-MgO particles of Ca–Mg/biochar could reduce the negative interaction effects of coexisting ions. The P releasing amounts of postsorption Ca–Mg/biochar were in the order of Ca–Mg/B600 > Ca–Mg/B450 > Ca–Mg/B300. Results revealed that postsorption Ca–Mg/biochar can continually release P and is more suitable for an acid environment.     

典型喀斯特小流域水文水化学过程对旱季暴雨的响应

通过定位监测和样品跟踪采集,在旱季对喀斯特小流域连续20天无前期降雨的一场暴雨(累计降雨量64mm)水文水化学过程进行了动态监测,并分析了相关的影响因素。结果表明,小降雨事件(8.5mm)未能引起溪流水位、电导率及温度的明显变化,而当累计降雨量达到35.5mm后溪流水开始响应。此后,溪流水文水化学参数对降雨快速响应,除硝态氮外,电导率(EC)、δ18 O、Ca2+迅速降至最低值,雨水稀释作用对其水化学变化起主要作用。通过对溪流新旧水比例进行划分发现,降雨前期和后期,溪流以旧水补给为主,而在水位快速上涨阶段,新水比例达到34%左右。两次降雨过程中,在溪流水水位升高的情况下,水体中硝态氮浓度仍然表现出高于雨前浓度的趋势。该研究为该区旱季小流域水资源利用和污染物防治方面提供了一定理论依据。     

Distribution of uranium isotopes in surface water of the Llobregat river basin (Northeast Spain)

A study is presented on the distribution of ²³⁴U, ²³⁸U, ²³⁵U isotopes in surface water of the Llobregat river basin (Northeast Spain), from 2001 to 2006. Sixty-six superficial water samples were collected at 16 points distributed throughout the Llobregat river basin. Uranium isotopes were measured by alpha spectrometry (PIPS detectors). The test procedure was validated according to the quality requirements of the ISO17025 standard. The activity concentration for the total dissolved uranium ranges from 20 to 261 mBq L⁻¹. The highest concentrations of uranium were detected in an area with formations of sedimentary rock, limestone and lignite. A high degree of radioactive disequilibrium was noted among the uranium isotopes. The ²³⁴U/²³⁸U activity ratio varied between 1.1 and 1.9 and the waters with the lowest uranium activity registered the highest level of ²³⁴U/²³⁸U activity ratio. Correlations between uranium activity in the tested water and chemical and physical characteristics of the aquifer were found.     

钙、镁离子在水流作用下对铜绿微囊藻生长的影响

为了解在"引江济太"过程中大量钙、镁离子的引入对铜绿微囊藻生长的影响,本实验在控制温度和光照条件下,室内模拟不同钙、镁离子浓度在两个特征流速5 cm/s和15 cm/s下微囊藻的生长。实验结果表明,微囊藻藻密度随钙、镁离子浓度的增加而增加,流速在15cm/s下微囊藻最大藻密度(9 236.4×104cell/mL)是流速为5 cm/s下最大藻密度(2 873.72×104cell/mL)的3倍,流速为15 cm/s下微囊藻最大比增长速率均较5 cm/s下的高。这可能是在水流产生的剪切力作用下藻细胞胞外多糖增加,粘附更多的钙、镁离子更利于钙、镁离子迁移到胞内,同时胞外附着的钙、镁离子尤其钙离子形成桥联,使微囊藻细胞形成群体产生微环境利于微囊藻的生长。水流对微囊藻利用钙、镁离子有重要的影响,这为有效调水抑制蓝藻生长提供科学依据。     

千岛湖水体氮的垂向分布特征及来源解析

选取千岛湖水深0.2,5,10,20,30和40m处水样进行分析,利用氮氧同位素和稳定同位素模型（SIAR）研究千岛湖水体氮（N）的垂向分布特征,分析水体N的来源并计算各N源的贡献率.结果表明,硝酸盐（NO₃^-）和溶解性有机氮（DON）是千岛湖水体总溶解氮（TDN）的主要形式,分别占溶解态N的57.9%和39.7%.千岛湖水体δ¹⁵N-NO₃^-和δ¹⁸O-NO₃^-的平均值分别为4.5‰和4.3‰.上层水体（0~10m）中,硝化作用和浮游植物的同化作用共同控制水体N的形态组成和氮氧同位素值（δ¹⁵N-NO₃^-和δ¹⁸O-NO₃^-）的变化.中层水体（10~30m）中,硝化作用是主要的生物地球化学过程,使得水体NO₃^-含量增加而δ¹⁸O-NO₃^-值减小.底层水体（30~40m）受到硝化作用、底泥N释放和反硝化作用的共同影响.化肥是千岛湖水体NO₃^-的最主要来源,在S1和S2处的贡献率分别为51.9%和30.6%.新安江上游的农业面源污染使得S1处化肥贡献率远高于S2.土壤N是仅次于化肥的第二大水体NO₃^-来源,在S1和S2处的贡献率分别为17.8%和27.8%.此外,底泥对底层水体NO₃^-的贡献不可忽视.     

氮和氧同位素示踪伊洛河河水硝酸盐来源及转化过程

河流硝酸盐(NO^-₃)浓度及氮和氧同位素组成(δ¹⁵N-NO^-₃和δ¹⁸O-NO^-₃)可以辨识河水NO^-₃受自然过程和人为输入的影响,但流域不同土地利用方式对河水NO^-₃来源及转化过程的影响尚不明确,特别是山区人为输入对河水NO^-₃的影响仍不清楚.选择土地利用空间异质性显著的伊河和洛河作为研究对象,借助水体水化学组成,氢氧同位素(δD-H₂O和δ¹⁸O-H₂O)、δ¹⁵N-NO^-₃和δ¹⁸O-NO^-₃,辨识不同土地利用方式影响下河水NO^-₃来源及...     

Human teeth as historical biomonitors of environmental and dietary lead: some lessons from isotopic studies of 19th and 20th century archival material

The lead isotopic composition of various sections (crown, crown base, root) of teeth was determined in specimens collected from 19th century skulls preserved in museum collections and, upon extraction or exfoliation, from humans of known ages residing in Scotland in the 1990s. For most 20th century samples, calculation of accurate crown-complete or root-complete dates of tooth formation ranging from the 1920s to the 1990s enabled comparison of ²⁰⁶Pb/²⁰⁷Pb ratios for teeth sections (crown base root) with corresponding decadally averaged data for archival herbarium Sphagnum moss samples. This showed that the teeth sections had been significantly influenced by incorporation of non-contemporaneous (more recent) lead subsequent to the time of tooth formation, most probably via continuous uptake by dentine. This finding confirmed that separation of enamel from dentine is necessary for the potential of teeth sections as historical biomonitors of environmental (and dietary) lead exposure at the time of tooth formation to be realised. Nevertheless, the mean 19th century value of 1.172±0.007 for the ²⁰⁶Pb/²⁰⁷Pb ratio in teeth was very similar to the corresponding mean value of 1.173±0.004 for 19th century archival moss, although relative contributions from environmental sources – whether direct, by inhalation/ingestion of dust contaminated by local lead smelting (²⁰⁶Pb/²⁰⁷Pb~1.17) and coal combustion (²⁰⁶Pb/²⁰⁷Pb~1.18) emissions, or indirect, through ingestion of similarly contaminated food – and drinking/cooking water contaminated by lead pipes of local origin, cannot readily be determined. In the 20th century, however, the much lower values of the ²⁰⁶Pb/²⁰⁷Pb ratio (range 1.100–1.166, mean 1.126±0.013, median 1.124) for the teeth collected from various age groups in the 1990s reflect the significant influence of imported Australian lead of lower ²⁰⁶Pb/²⁰⁷Pb ratio (~1.04) and released to the environment most notably through car-exhaust emissions arising from the use of alkyl lead additives (²⁰⁶Pb/²⁰⁷Pb~1.06–1.09) in petrol in the U.K. from ca. 1930 until the end of the 20th century.     

矿用聚氨酯注浆材料阻燃及加固性能研究

为获得压缩强度和阻燃性能兼顾的聚氨酯注浆材料,通过L9(34)正交试验,研究Mg(OH)2含量、甲基膦酸二甲酯(DMMP)含量、异氰酸酯指数、辛酸亚锡含量对聚氨酯注浆材料的阻燃性能及压缩性能的影响。获得这种聚氨酯注浆材料的最佳制备条件。对比分析最佳制备条件试样及不加阻燃剂试样的热稳定性。结果表明:DMMP含量和Mg(OH)2含量对平均燃烧时间影响显著;Mg(OH)2还有补强加固作用,对压缩强度影响最为显著,其次为异氰酸酯指数。在Mg(OH)2,DMMP,辛酸亚锡质量分数分别为16%,24%和0.4%,异氰酸酯指数为1.10时,聚氨酯注浆材料兼顾阻燃性能和压缩性能,平均燃烧时间为13.9 s,压缩强度为19 MPa,其热稳定性明显优于不添加阻燃剂样品。     

低压离子色谱法测定水和酸雨样品中的Li~+,Na~+,NH_4~+,K~+,Ca~(2+)和Mg~(2+)离子

本文介绍了低压离子色谱仪测定水样(井水、湖水、矿泉水、自来水)和酸雨中锂、钠、铵、钙、钾和镁离子的方法、欲测阳离子在阳离子交换柱上被分离,分别用1.4mmol·1~(-1)HNO_3和0.6mmol·1~(-1)乙二胺+1.2mmol·1~(-1)HNO_3溶液作流动相,流速为1.6ml·min~(-1).各离子的流分用电导检测.进样量为10μl时,Li~+,Na~+,NH_4~+,K~+,Ca~(2+)和Mg~(2+)离子的检出限(2倍噪音比),分别为0.020,0.050,0.100,0.250,2.5和1.0μg·ml~(-1).