不同施氮量下水稻分蘖期光合碳向土壤碳库的输入及其分配的量化研究：13C连续标记法

应用稳定同位素13C-CO2连续标记技术,通过室内密闭培养试验研究不同施氮处理下(依次为N0,N10,N20,N40,N60)水稻分蘖期光合碳向土壤碳库的输入及其分配特征.结果表明,连续标记培养18 d后,水稻地上部和根系的干物质累积量分别为1.58~4.35 g·plot-1和1.05~2.44 g·plot-1,水稻植株生物量受施氮处理显著影响,且随着施氮量增加而增加,即N60>N40>N20>N10>N0.水稻整个分蘖期内分别有44.0~157.6 g·plot-1和8.3~49.4 g·plot-1的光合碳进入水稻地上部和根系.不同施氮水平下,种植水稻的土壤有机碳(13C-SOC)、可溶性有机碳(13C-DOC)和微生物量碳(13C-MBC)的分配量均显著高于CK处理(不种植水稻且不施N).种植水稻的土壤13C-SOC含量范围为11.1~23.7 g·plot-1,占总净同化量的10.2%~18.1%.对于活性碳库,CK处理的土壤13C-DOC和13C-MBC含量分别为3.50μg·kg-1和88.9μg·kg-1,种植水稻处理的土壤13C-DOC、13C-MBC含量范围为4.82~14.51μg·kg-1、526.1~1 478.8μg·kg-1.土壤13C-SOC、13C-DOC和13C-MBC含量受施氮处理显著影响(P<0.05),且与植物生物量呈显著正相关关系.因此,水稻分蘖期光合碳的地下部输入有利于土壤有机碳的累积,施氮能够促进水稻新鲜根际碳的沉积,且高N水平下根际沉积碳量高于低N和中量N水平.     

Size distribution, characteristics and sources of heavy metals in haze episod in Beijing

Size segragated samples were collected during high polluted winter haze days in 2006 in Beijing, China. Twenty nine elements and 9 water soluble ions were determined. Heavy metals of Zn, Pb, Mn, Cu, As, Cr, Ni, V and Cd were deeply studied considering their toxic effect on human being. Among these heavy metals, the levels of Mn, As and Cd exceeded the reference values of National Ambient Air Quality Standard （GB3095-2012） and guidelines of World Health Organization. By estimation, high percentage of atmospheric heavy metals in PM2.5 indicates it is an effective way to control atmospheric heavy metals by PM2.5 controlling. Pb, Cd, and Zn show mostly in accumulation mode, V, Mn and Cu exist mostly in both coarse and accumulation modes, and Ni and Cr exist in all of the three modes. Considering the health effect, the breakthrough rates of atmospheric heavy metals into pulmonary alveoli are： Pb （62.1%） 〉 As （58.1%） 〉 Cd （57.9%） 〉 Zn （57.7%） 〉 Cu （55.8%） 〉 Ni （53.5%） 〉 Cr （52.2%） 〉 Mn （49.2%） 〉 V （43.5%）. Positive matrix factorization method was applied for source apportionment of studied heavy metals combined with some marker elements and ions such as K, As, SO42- etc., and four factors （dust, vehicle, aged and transportation, unknown） are identified and the size distribution contribution of them to atmospheric heavy metals are discussed.     

地表水体中同时分析18种糖皮质激素方法的建立

建立了一种采用固相萃取-超高效液相色谱串极质谱联用系统(UPLC-MS/MS)同时测定地表水体中18种糖皮质激素的高灵敏分析方法.样品经过HLB固相萃取柱富集净化、V(乙腈)/V(乙酸乙酯)=1∶1,洗脱后,用UPLC-MS/MS测定.流动相为甲醇和0.1%乙酸水溶液(体积比),采用梯度洗脱,实现了18种目标物质的基线分离,线性范围为1.0~1 000μg·L-1.实际水样的加标回收率为65%~108%.整个分析的方法检出限(MDL)除醋酸可的松和醋酸氢化可的松为10 ng·L-1外,其他均在0.10 ng·L-1和1.0 ng·L-1之间.应用此方法于北京地表水体5个样品,检测到8种糖皮质激素,浓度范围0.20~476ng·L-1,其中曲安西龙、曲安奈德、醋酸氢化可的松和丙酸氯倍他索在地表水中首次检出,证明了该方法的有效性.     

硫磺回收装置腐蚀原因及防护措施

针对国内硫磺回收装置实际生产中存在的设备腐蚀问题,根据不同的腐蚀机理进行了腐蚀分类,分析了腐蚀原因并提出了具体的防护措施.     

常减压蒸馏装置的清洁生产

中国石油天然气股份有限公司辽河石化分公司南蒸馏装置于2000年底改造,2001年5月开车成功.由于需要装置改加工低凝环烷基原油,这种原油具有酸值高、体积质量大、黏度大,腐蚀性极强.     

骆马湖泥-水界面磷铁硫原位同步变化特征

利用薄膜梯度扩散（DGT）原位采样装置获取了骆马湖全湖8个典型湖区泥-水界面（SWI）活性磷（P）、铁（Fe）、硫（S）垂向分布信息，据此定量估算三者交换通量.结果表明，骆马湖沉积物剖面P、Fe、S浓度范围分别为0~2.05，0~11.10和0.01~0.63mg/L，并在微小尺度呈高度空间异质性.在水平方向上活性P、Fe主要表现为西北湖区高于东南湖区，而活性S则未表现出明显的分布规律；就垂直剖面而言，活性P、Fe、S自界面向下呈升高趋势，并在60mm深度内出现峰值，且活性P和Fe剖面呈明显的同步变化特征；活性P、Fe在多数点位具有显著的正相关性（r>0.65，P<0.01），且各采样点沉积物中的总铁与总磷比值[w（∑Fe）/w（∑P）]均高于15，这表明Fe的地球化学循环过程对于骆马湖内源磷释放起重要控制作用；8个采样点样品中活性P、Fe、S交换通量分别为0.066~0.698，1.671~5.592和0.007~0.071mg/（m²·d），表明P、Fe、S由沉积物向水体释放.西北湖区表现出较高的P通量和活性P浓度，这可能会增加南水北调过程中水质污染的风险，应予以重视.以上结果支持了P、Fe耦合释放机制，明确了骆马湖SWI的活性P、Fe、S迁移特征.     

Coalbed methane produced water in China: status and environmental issues

As one of the unconventional natural gas family members, coalbed methane (CBM) receives great attention throughout the world. The major associated problem of CBM production is the management of produced water. In the USA, Canada, and Australia, much research has been done on the effects and management of coalbed methane produced water (CMPW). However, in China, the environmental effects of CMPW were overlooked. The quantity and the quality of CMPW both vary enormously between coal basins or stratigraphic units in China. The unit produced water volume of CBM wells in China ranges from 10 to 271,280 L/well/day, and the concentration of total dissolved solids (TDS) ranges from 691 to 93,898 mg/L. Most pH values of CMPW are more than 7.0, showing the alkaline feature, and the Na-HCO₃ and Na-HCO₃-Cl are typical types of CMPW in China. Treatment and utilization of CMPW in China lag far behind the USA and Australia, and CMPW is mainly managed by surface impoundments and evaporation. Currently, the core environmental issues associated with CMPW in China are that the potential environmental problems of CMPW have not been given enough attention, and relevant regulations as well as environmental impact assessment (EIA) guidelines for CMPW are still lacking. Other potential issues in China includes (1) water quality monitoring issues for CMPW with special components in special areas, (2) groundwater level decline issues associated with the dewatering process, and (3) potential environmental issues of groundwater pollution associated with hydraulic fracturing.     

Past, Status Quo and Future of China’s Territorial Planning

Since 1949, China has witnessed four development stages of territorial planning. （1） In the 1950s the territorial planning got its start. （2） From the 1960s to 1970s territorial planning declined. （3） From, the 1980s to 1990s the first major tide of territorial planning began. （4） From the end of the 1990s to recent times the new round of territorial planning is under deliberation. Since 1998, the Ministry of Land and Resources has carried out some related work, especially in organizing pilot projects, and early research on the new round of national territorial planning. According to the need for economic and social development and the current conditions in China, it is the appropriate for China to carry out the new round of territorial planning. However, the government should correctly consider the correlations between territorial planning and other plan- nings, and take appropriate development action, e.g. stressing main points for the basis of overall planning, building a territorial planning system that coordinate with national conditions, strengthening research on various supportive measures of territorial planning, summarizing and upgrading experiences obtained in pilot projects, strengthening international exchange and training talented personnel.     

Identification of main influencing factors of life cycle CO2 emissions from the integrated steelworks using sensitivity analysis

The amount of CO₂ emissions from steelworks accounts for a great share of the total CO₂ emissions from industry in China. Thus, reducing CO₂ emissions from steelworks is urgent for China's environmental protection and sustainable development. This study aims at identifying factors that influence CO₂ emissions from steelworks and proposing measures to reduce CO₂ emissions. The life cycle inventory (LCI) of iron and steel products implies the relationship between the CO₂ emissions of the steelworks and the input variables of the LCI. The Tornado Chart Tool is utilized to calculate the variation of CO₂ emissions caused by the change of each input variables of LCI. Then, mean sensitivity of each input variable is calculated and the ranking criterion developed is used to identify the main factors influencing the integrated steelworks. Subsequently, measures for reducing CO₂ emissions are proposed. The results indicate that the very important influencing factors of CO₂ emissions in steelworks are the CO₂ emission factor of Blast Furnace Gas (BFG), liquid steel unit consumption of continuous casting, continuous casting slab unit consumption of hot rolling and hot metal ratio of steel making. Consequently, many efficient measures for reducing CO₂ emissions have been proposed, such as removing CO₂ contained in BFG, decreasing the hot metal ratio of Basic Oxygen Furnace (BOF), recycling BFG, optimizing the products' structure, etc.     

喀斯特水库碳、硅耦合循环:以红枫湖、普定水库和平寨水库为例

通过研究红枫湖、普定水库和平寨水库三个喀斯特水库的碳、硅循环,探讨了水库碳-硅循环的耦合关系。藻类光合作用导致表层水体溶解硅(DSi)及溶解无机碳(DIC)的亏损;当DSi供应不足时,硅藻生长繁殖大量消耗DSi,导致DSi相对DIC快速亏损。沉降颗粒物中内源有机碳含量越高,生物硅(BSi)及有机碳(OC)含量越高,但OC/BSi受控于硅藻对沉积物有机碳贡献率,且与之呈反比。生物硅与有机碳含量之比K值(K=BSi/OC)可作为硅藻贡献率的潜在替代指标,并与之呈正相关;生物硅与内源有机碳(OC_(auto))含量之比K_(auto)值(K_(auto)=BSi/OC_(auto))可作为水体富营养化程度的潜在替代指标,并与富营养化程度呈负相关。