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61.
MethaneemissioninaricefieldofThailand¥RongXiang;Chuen-HowNg(EnvironmentalEngineeringProgram,SchoolofEnvironment,ResourcesandD... 相似文献
62.
在立式管状电加热炉上对合山高硫煤在不同的气氛、温度以及Ca/S比的条件下进行了动态燃烧实验,对收集的气体产物进行了红外光谱分析,并讨论了CO2浓度以及温度等因素对SO2释放的影响。结果表明:不同浓度的CO2气氛对煤燃烧过程中硫的释放以及石灰石的固硫效率有着不同的影响,在高于900℃以后,较之空气气氛下,无论是否存在钙基固硫剂,其它三种02/C02气氛下S02的排放量都比较低,且在不同C02浓度下,温度对S02的排放影响不一致。 相似文献
63.
64.
太原市工业区大气中TSP浓度及元素成分分析 总被引:3,自引:0,他引:3
采用校正空白称量法对太原市工业区大气中TSP浓度进行了测定分析,对该区大气TSP浓度随时间变化的规律,超标情况及污染特征进行了研究,同时测定了TSP中Cr、Pb等12种元素的含量。 相似文献
65.
L. V. Mukhortova I. N. Bezkorovainaya 《Mitigation and Adaptation Strategies for Global Change》2006,11(1):191-202
The evaluation of biospheric role of the boreal forests in the accumulation of carbon is connected with the evaluation of
organic matter (OM) pool in soils. The research sites were larch forests, they are situated on Nizhne-Tungusskoe Plateau.
Larch forests of feather-moss and lichen types (110 and 380 years old) were formed on 'ochric podbur' soils. Litter stocks
are 3.5–4.5 kg m− 2 with thickness 10–25 cm. Cryomezomorphic northern taiga soils contains 38–73 t (carbon) ha− 1. Pool of fast mineralized OM has average value 38.1 t (carbon) ha− 1, including 20.5 and 6.4 t (Carbon) ha− 1 of labile compounds on surface and in the soil, and 11.2 t (carbon) ha− 1 of mobile OM. Microbial mass reaches 1.78–3.47 t (carbon) ha− 1, its proportion is 3.6–4.9% of the total OM carbon. Zoomass of feather-moss larch forest is 0.20–0.61 * 10− 2, in lichen larch forest −0.01–0.07 * 10− 2 t (carbon) ha− 1. A pool of resistant to biological decomposition and bonded to mineral soil matrix OM is 17.7 t (carbon) ha− 1 and it varies from 18.6 to 29.0 in feather-moss larch forest, and from 6.4 to 17.0 t (carbon) ha− 1 in lichen larch forest. Two-years field experiment has been performed to determine transformation rates of various plant
litter fractions and to clarify the role of soil biota in these processes. The results showed participation of all biota groups
in the decomposition of plant residues caused weight loss of larch-needles and root mortmass. Isolation of organic matter
from all-size invertebrate groups leads to some decrease of decomposition activity. 相似文献
66.
作为世界上规模最大的一个超高压变质带,大别山超高压变质杂岩是扬子板块 与中朝板块在三叠纪碰撞造山的产物,表现为扬子板块呈北北东向斜向俯冲到中朝板块之下。 超高压变质杂岩的折返机制是个复杂的动力学过程,折返速率也随时间推移而变慢。早期阶段 (三叠纪-早侏罗纪)同碰撞期浮力驱动下高压-超高压变质杂岩在俯冲带内沿道冲-韧性剪 切断裂快速挤侵(extrusio)到地壳层位,折返速率高达4mm/年;中期伴随着巨厚造山带山根的 拆沉,上部发生拉张塌陷,使超高压变质杂岩进一步减压,但折返速率缓慢,~(40)Ar/~(39)Ar年代学显 示117Ma前它们仍处在地壳的较深部;晚期伴随着晚侏罗-早白垩纪花岗质岩浆的上升侵位, 超高压变质杂岩进一步抬升,同时低角度正断层发育,此阶段的折返机制类似于变质核杂岩模 型。整个折返过程中剥蚀一直在起作用。 相似文献
67.
Given the key role of biogenic volatile organic compounds(VOCs) to tropospheric chemistry and regional air quality, it is important to generate accurateVOCs emission inventories. However, only a less fraction of plant species, in temperate grassland of Inner Mongolia, has been characterized by quantitative measurements. A taxonomic methodology, which assigns VOCs measurements to unmeasured species, is an applicable and inexpensive alternation for extensive VOCs emission survey, although data are needed for additional plant families and genera to further validate the taxonomic approach in grassland vegetation. In this experiment, VOCs emission rates of 178 plant species were measured with a portable photoionization detector( PID). The results showed the most of genera and some families have consistent feature of their VOCs emission, especially for isoprene, and provide the basic premise of taxonomic methodology to develop VOCs emission inventories for temperate grassland. Then, the taxonomic methodology was introduced into assigning emission rate to other 96 species, which no measured emission rates available here. A systematical emission inventory of temperate grassland vegetation in Inner Mongolia was provided and further evidence that taxonomy relationship can serve as a useful guide for generalizing the emissions behavior of many, but not all, plant families and genera to grassland vegetation. 相似文献
68.
A baseline for a project consists of estimates of annual emissions of greenhouse gases (GHG) for a given time period without implementing the project. A general three-step process for determining the baseline is suggested. The emission reduction of the project is given by the difference between the baseline and the monitored annual emissions. A preferred method, direct measurement of the emission reduction, is possible for some types of projects. Methods for estimating the annual baseline emissions are not necessary for the latter category, and a definition of this project category is suggested. IPCC Guidelines for National GHG Inventories categorise the emission sources so that only direct emissions from consumption of fuel and feedstock are calculated. There are thus no emission factors for indirect emissions (e.g. electricity consumption or km transported) or emission factors that depend on technology only, independent of consumption of fuel and feedstock. Technology-dependent emission factors may thus need to be developed for estimating indirect emissions and multi-project baselines. Consistency should be sought with the IPCC Guidelines when estimating annual baseline emissions and in monitoring project emissions to ensure comparability with the National Inventories. 相似文献
69.
阐述了石英表面配合物和溶解动力学机理之间的关系,指出了石英的反应性主要受负电性表面物种的控制,从而导致电解质、离子强度、pH等因素对石英溶解的催化效应.溶解达率的提高与反应活化能的降低成活化熵的增大有关。最后,介绍了在过渡态理论和表面反应模型基础上建立的石英溶解速率方程。 相似文献
70.
排污权交易在中国的试点过程中,显现了强大的生命力,然而,由于对排污权交易基础理论理解的偏差,导致了实践层面上的缺陷,如排污权初始分配是否应该有偿的问题;排污权商品再分配价格应不应该包括正的外部效应价值问题;在排污权交易制度改革与中国其他制度的改革(现行税制改革、绿色GDP的推行)进行中出现的不协调的问题. 相似文献