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961.
962.
Johannes Lehmann John Gaunt Marco Rondon 《Mitigation and Adaptation Strategies for Global Change》2006,11(2):395-419
The application of bio-char (charcoal or biomass-derived black carbon (C)) to soil is proposed as a novel approach to establish
a significant, long-term, sink for atmospheric carbon dioxide in terrestrial ecosystems. Apart from positive effects in both
reducing emissions and increasing the sequestration of greenhouse gases, the production of bio-char and its application to
soil will deliver immediate benefits through improved soil fertility and increased crop production. Conversion of biomass
C to bio-char C leads to sequestration of about 50% of the initial C compared to the low amounts retained after burning (3%)
and biological decomposition (< 10–20% after 5–10 years), therefore yielding more stable soil C than burning or direct land
application of biomass. This efficiency of C conversion of biomass to bio-char is highly dependent on the type of feedstock,
but is not significantly affected by the pyrolysis temperature (within 350–500 ∘C common for pyrolysis). Existing slash-and-burn systems cause significant degradation of soil and release of greenhouse gases
and opportunies may exist to enhance this system by conversion to slash-and-char systems. Our global analysis revealed that
up to 12% of the total anthropogenic C emissions by land use change (0.21 Pg C) can be off-set annually in soil, if slash-and-burn
is replaced by slash-and-char. Agricultural and forestry wastes such as forest residues, mill residues, field crop residues,
or urban wastes add a conservatively estimated 0.16 Pg C yr−1. Biofuel production using modern biomass can produce a bio-char by-product through pyrolysis which results in 30.6 kg C sequestration
for each GJ of energy produced. Using published projections of the use of renewable fuels in the year 2100, bio-char sequestration
could amount to 5.5–9.5 Pg C yr−1 if this demand for energy was met through pyrolysis, which would exceed current emissions from fossil fuels (5.4 Pg C yr−1). Bio-char soil management systems can deliver tradable C emissions reduction, and C sequestered is easily accountable, and
verifiable. 相似文献
963.
本文讨论土壤、农业与全球气候变化的相互关系及相互影响,包括土壤圈、农业生产活动对全球气候变化的影响,以及全球气候变化对农业产生的直接和间接影响.并对引起CO2浓度上升、气温增高和水文条件改变等对世界农业和中国农业的正、负面效应进行预测、评估. 相似文献
964.
This study investigates energy dissipation due to air bubble entrainment for three typical phenomena; a hydraulic jump, a
2-D vertical plunging jet and a vertical circular plunging jet into water. A simple model is presented here which enables
to estimate the energy transformation and dissipation achieved by air bubbles quantitatively for three above phenomena. The
average rate of energy dissipation by air bubbles obtained from the experimental data are 25%, 1.4%, and 2.15% with respect
to total energy loss for the hydraulic jump, 2-D vertical plunging jet and vertical circular plunging jet, respectively. 相似文献
965.
Weapon size versus body size as a predictor of winning in fights between shore crabs, Carcinus maenas (L.) 总被引:4,自引:0,他引:4
Lynne U. Sneddon Felicity A. Huntingford Alan C. Taylor 《Behavioral ecology and sociobiology》1997,41(4):237-242
Relative body size (carapace width) and weapon size (chela length) were used as indicators of resource holding potential (RHP)
in the agonistic behaviour of male shore crabs, Carcinus maenas (L.). Weapon size was found to be a more reliable predictor of the outcome of pairwise fights than body size. Crabs with
longer chelae than their opponents were more likely to win fights than crabs with relatively larger bodies. Body size had
less influence on the outcome of fights. Relative body and weapon size did not influence initiation of contests but did affect
the likelihood of winning; however, this was significant only for weapon size. Winning crabs had heavier claws with greater
surface area than losing crabs. There was no relationship between relative size and fight duration. The frequency of cheliped
display increased with chela length and win- ners performed significantly more displays than losers.
Received: 5 February 1997 / Accepted after revision: 20 May 1997 相似文献
966.
为更系统地归纳安全氛围与安全绩效的关系,探究安全氛围、安全绩效及安全结果间的影响机制,采用Meta分析方法,通过2000—2020年54篇文献的55个独立研究样本进行定量综合分析,并进一步探讨安全氛围与安全绩效各维度间的关系,同时运用Meta二元回归探究潜在调节变量对2者间关系的调节作用。结果表明:安全氛围显著正向影响安全绩效,在高危行业中安全氛围对安全绩效影响更大;安全氛围与安全参与、安全遵守均显著正相关,且安全氛围对安全参与的影响强于对安全遵守的影响;安全氛围和安全绩效均与安全结果显著负相关,且安全绩效对安全结果的影响强于安全氛围对安全结果的影响。 相似文献
967.
为解决尾矿库安全隐患及风险,应用基于证据(Evidence-based)方法和事故树分析模型,辨识并表征尾矿库事故影响因素、隐患及耦合状态,根据事件发生可能性、潜在后果严重性和受体暴露程度相关独立参数,给出尾矿库事故风险表征方法,建立尾矿库事故多情景、多阶段(3段)、多层次和多等级(4级)风险防控框架。结果表明:对尾矿库5类事故(溃坝、漫顶、渗流、输送冒漏、库区扬尘)进行分析,得出基本事件或蛰伏隐患对尾矿库事故结构重要度或影响程度,给出尾矿库事故风险3维表征方法,并结合巴西布鲁马迪尼奥尾矿库进行实例应用,确定尾矿库风险等级(最高级4级),验证方法可行性与有效性。研究结果可为尾矿库减灾防灾提供理论支撑与实践指导。 相似文献
968.
Ram Ranjan 《Mitigation and Adaptation Strategies for Global Change》2008,13(4):401-418
This paper explores the role of risk perceptions in influencing public policy related to global warming. It solves for the
optimal paths for emissions, abatement and investment in pollution-eliminating research by incorporating perceived risks into
public decision making. It also compares the impact of differential risk perceptions on international collaboration on carbon
abatement. Key findings are that the perception of risks related to environmental damages and technological breakthroughs
plays an important role in determining the level of mitigation efforts. A high level of perceived risk of environmental damages
discourages investment in pollution-eliminating research as there are few benefits from eliminating pollution after damages
are realized. Other options that allow for sequestering carbon from the atmosphere may still remain viable. Another key finding
is that when it comes to effort sharing between nations, differential mitigation efforts are primarily caused due to the differences
in abatement technology, benefits from emissions and research capabilities. However, such differences could be accentuated
or mitigated depending upon the differences in risk perception of developed and developing countries. 相似文献
969.
全球气候变暖成因分析 总被引:18,自引:1,他引:17
论述了太阳辐射、大气环流和地表状况是形成气候的3个基本因素.此外,还有人类活动、太阳活动、火山活动等影响气候变化的第4类因子.影响全球气候变暖的因素既有自然因素,也有人为因素.但导致近百年全球气候持续变暖的主要因素是人为因素(人类活动),即自19世纪末工业革命后,世界各国工业化、城市化快速发展,使大气中CO2等“温室效应“气体持续增加,而森林植被遭到大量砍伐和破坏,全球森林植被覆盖率持续下降,平衡大气中CO2与O2的生态功能不断下降,结果导致全球“温室效应“持续增强,使近百年来全球气候持续变暖.自然因素太阳活动对全球气候变暖的影响是周期性而不是持续性的.太阳活动增强期(高峰期)有增温作用,减弱期(低谷期)有降温作用,对全球气候变暖有影响,但比起人类活动造成的CO2等气体“温室效应“持续增强对气候持续变暖的影响相对较小. 相似文献
970.