喀斯特森林植被自然恢复过程中土壤可矿化碳库特征

2011年9月,采用空间代替时间方法,研究了茂兰自然保护区喀斯特森林自然恢复过程中土壤可矿化碳库的特征.结果表明: 研究期间,喀斯特森林自然恢复过程中不同深度土壤的总有机碳含量、可矿化碳含量和矿化速率随土层加深而减少,随恢复的进程而增加;累积矿化排放量及其速率随恢复的进程增加,其速率随培养时间延长而减小;矿化率随恢复的进程增加,而随土层加深的变化不明显;qCO₂值随恢复的进程和土层加深而递减;土壤可矿化碳与凋落物现存量及其分解质量损失率分别呈负相关(r=-0.796)和正相关(r=0.924);土壤生境由早期干扰强烈转向中后期日趋稳定,土壤的固碳能力由早期差、潜力大转向中后期强、潜力小.     

Structural stability and buckling analysis of a series of carbon nanotorus using molecular dynamics simulations

Based on molecular dynamics (MD) simulations, the buckling analysis of a perfect carbon nanotorus is presented herein. First of all, the minimum length of single-walled carbon nanotubes (SWCNTs) with different radii is determined at which perfect toroidal CNTs can be formed without any ripple at the inner side of the rings. According to the results, by increasing the radius of SWCNT (r), the radius of its corresponding perfect nanotorus (R) increases. Also, for SWCNTs with various lengths, it is found that the buckling force and strain of related carbon nanotoruses increase by increasing R/r. In addition, as the perfect toroidal CNTs are arranged vertically in a column form in accordance with two different schemes, the effects of increasing the radius (R) and the number of carbon nanotoruses (the height of the column made by nanotoruses) on the buckling force and strain are investigated. Based on the results, as a fixed number of carbon nanotoruses with the same radius are arranged vertically in the column form, the buckling force and strain increase by increasing R/r. By contrast, increasing the height of the column made by carbon nanotoruses with similar radius leads to the reduction of buckling force and strain.     

长期植稻年限序列水稻土团聚体有机碳分布特征

通过开展有机质物理分组试验,研究了杭州湾南岸不同植稻年限序列水稻土有机碳含量的粒级分布变化特征.结果表明: 各植稻年限耕层水稻土中,土壤团聚体主要分布在微团聚体(<0.25 mm)中,其中大微团聚体(0.053～0.25 mm)随着植稻年限的增加而减少;在微团聚体(0.053~0.25 mm,<0.053 mm)中,有机碳含量随着植稻年限的增加而增加,在0.053～2 mm粒径范围内,各粒级有机碳占总有机碳比例随着粒级的减小而增加,有机碳主要集中在大微团聚体(0.053～0.25 mm)中;随着种植年限的增加,颗粒有机碳含量减少.栽培年限长的水稻土比栽培年限短的水稻土碳封存量大,早期开垦的水稻土仍有很大的固碳潜力.     

长期植稻年限序列水稻土团聚体有机碳分布特征

通过开展有机质物理分组试验,研究了杭州湾南岸不同植稻年限序列水稻土有机碳含量的粒级分布变化特征.结果表明: 各植稻年限耕层水稻土中,土壤团聚体主要分布在微团聚体(<0.25 mm)中,其中大微团聚体(0.053～0.25 mm)随着植稻年限的增加而减少;在微团聚体(0.053~0.25 mm,<0.053 mm)中,有机碳含量随着植稻年限的增加而增加,在0.053～2 mm粒径范围内,各粒级有机碳占总有机碳比例随着粒级的减小而增加,有机碳主要集中在大微团聚体(0.053～0.25 mm)中;随着种植年限的增加,颗粒有机碳含量减少.栽培年限长的水稻土比栽培年限短的水稻土碳封存量大,早期开垦的水稻土仍有很大的固碳潜力.     

Effects of Surface Area and Flow Rate on Marine Bacterial Growth in Activated Carbon Columns

The colonization of granular activated carbon columns by bacteria can have both beneficial and potentially detrimental consequences. Bacterial growth on the carbon surface can remove adsorbed organics and thus partially regenerate the carbon bed. However, growth can also increase the levels of bacteria in the column effluents, which can adversely affect downstream uses of the treated water. This study of a sand column and several activated carbon columns demonstrated that considerable marine bacterial growth occurred in both sand and carbon columns and that this growth increased the number of bacteria in column effluents. Activated carbon supported approximately 50% more bacteria than did sand. Bacterial growth on activated carbon was reduced by increasing the flow rate through a carbon column and increasing the carbon particle size. Scanning electron micrographs showed that bacteria preferred to attach in the protected crevices on both the sand and carbon surface. The results of this study indicated that the colonization of activated carbon by marine bacteria was enhanced because of carbon's high surface area, its rough surface texture, and its ability to absorb organic materials.     

Polysaccharide hydrolysis accelerated by adding carbon dioxide under hydrothermal conditions

Polysaccharides such as agar, guar gum, starch, and xylan were hydrolyzed to produce mono- and oligosaccharides under hydrothermal conditions with and without carbon dioxide in a small batch reactor. The molecular weight distributions of the polysaccharide hydrolyzates shifted to lower molecular weights by increasing the carbon dioxide load, corresponding to higher pressures of carbon dioxide. For example, the yield of glucose produced from the hydrolysis of starch at 200 degrees C was increased significantly from 3.7% to 53.0% (on a carbon weight basis) of the initial polysaccharide by increasing carbon dioxide load in a reaction time of 15 min. Carbonic acid generated from water and carbon dioxide appeared to lower the pH of high-temperature and high-pressure water. Polysaccharide hydrolysis under hydrothermal conditions in the presence of carbon dioxide is an environmentally benign method to produce mono- and oligosaccharides because the process does not require the use of conventional acids and bases followed by neutralization and separation.     

活性炭对苦荞幼苗根系和叶片生理特性的影响

以山西省主栽苦荞品种‘黑丰1号’温室盆栽幼苗为材料,设置土壤活性炭含量分别为0(CK)、2.5(B2.5)、5.0(B5.0)、7.5(B7.5)、10(B10)g/kg共5个水平,研究土壤中施加活性炭后对苦荞幼苗根系及碳氮代谢、保护酶活性等指标的影响.结果显示:(1)随着活性炭施用比例的增加,苦荞幼苗根系生长指标和根系活力指标均呈先增后减的趋势,根平均直径呈先减后增的趋势,其中B5.0、B7.5处理的幼苗根系总长度、总表面积、总体积、活跃吸收面积、根尖数均显著高于对照,但B10处理的根系发育减弱.(2)随活性炭施用比例的增加,苦荞幼苗叶片蔗糖酶活性变化呈先增后减的趋势,同一处理水平条件下随苦荞的生长而逐渐下降;B2.5、B5.0处理苦荞幼苗叶片蔗糖酶活性和可溶性糖含量均比CK极显著增加,B7.5处理略有提高,B10处理差异不显著.(3)苦荞幼苗叶片谷氨酰胺合成酶(GS)活性随活性炭的增加基本呈上升趋势,而同一处理水平下随苦荞的生长而下降;叶片GS活性在B5.0、B7.5处理时比CK极显著提高,可溶性蛋白质含量在B7.5处理时也显著提高.(4)叶片保护酶SOD、POD、CAT活性随活性炭浓度的升高呈先升后降的变化趋势,而同一处理水平下各时期间变化不大;B2.5处理叶片的SOD、POD和CAT活性比对照显著增强.研究发现,适量施用活性炭(2.5～7.5g/kg)能有效促进苦荞幼苗碳氮代谢和保护酶活性,增强其根系活力.     

Mechanisms influencing physically sequestered soil carbon in temperate restored grasslands in South Africa and North America

Biogeochemistry - Sequestering carbon (C) into stable soil pools has potential to mitigate increasing atmospheric carbon dioxide concentrations. Carbon accrues in grassland soil restored from...     

Effects of soil strength on the relation of water-use efficiency and growth to carbon isotope discrimination in wheat seedlings

The ratio of carbon accumulation to transpiration, W, of wheat (Triticum aestivum L.) seedlings increased with increasing soil strength, measured as soil penetrometer resistance, and this was already apparent at the two leaf stage. The ratio was negatively correlated with carbon isotope discrimination, in accord with theory. This means that decrease in intercellular partial pressure of CO₂ accounted for an important part of the increase in W with increasing soil strength. Despite a lower CO₂ concentration in the leaves at high soil strength, assimilation rate per unit leaf area was enhanced. Greater ribulose 1,5-bisphosphate carboxylase activity confirmed that photosynthetic capacity was actually increased. This pattern of opposite variation of assimilation rate and of stomatal conductance is unusual. The ratio of plant carbon mass to leaf area increased markedly with increasing soil strength, mainly because of a greater investment of carbon into roots than into shoots. A strong negative correlation was found between this ratio and carbon isotope discrimination. For a given increase in discrimination, decrease in carbon mass per leaf area was proportionally larger than decrease in assimilation rate, so that relative growth rate was positively correlated to carbon isotope discrimination.     

农地利用碳强度及可持续性动态变化——以山东省平度市为例

以中国东部山东省平度市为案例区,通过识别重要的农地利用碳排放源和构建碳排放测算体系,包括农用化学物质投入间接碳排放、耗能碳排放、氮肥施用后导致的土壤直接N_2O释放、秸秆燃烧碳排放和牲畜养殖CH_4和N_2O排放,测算了1995—2013年农地利用的碳排放量;结合农产品产值分析了农地利用碳强度变化特征,结合农作物碳吸收分析了农地利用的碳可持续指数的变化规律。研究得出:(1)1995—2013年平度年均碳排放量的次序是:农资投入22.50万t牲畜养殖17.41万t秸秆燃烧6.62万t,其中秸秆燃烧碳排放呈逐年增加态势,而农资投入和畜牧养殖均呈逐年减少趋势。(2)平度农地利用碳强度变化结果表明,农产品产值增加速度超过农地利用碳排放速度,单位产值碳排放已从1995年的1.24 t/元降至2013年的0.35 t/元。(3)碳可持续性指数变化特征表明,平度农地利用过程中碳吸收大于碳排放,且碳可持续性指数以年均7.12%速率增长,故平度农作物生产期的碳吸收能够完全消纳农地利用过程中所产生碳排放。该研究不仅为中小尺度以及我国东部区域的农地利用碳排放及可持续发展提供科学依据,而且有益于推进我国农业的碳减排,并为国际全球环境变化人文因素计划中LUCC、碳循环等重大问题的研究提供基本素材。     

赣中亚热带森林植被碳储量

利用已发表的乔木生物量回归模型（乔木层）和样方收获法（灌木层、草本层）,沿江西省泰和县灌溪乡千烟洲至井冈山市大井林场一线,采用样带法研究了赣中地区亚热带湿润气候下的植被群落碳储量及其分配规律。研究结果表明：群落碳储量绝大部分集中于乔木层。乔木层单位面积碳储量与乔木密度的幂指数为一0．0756。碳储量的空间变化规律表现为植被的碳密度与经度之间没有显著的相关性,而与纬度和海拔间均存在着显著的相关关系,表现为随着纬度和海拔增加植被碳密度递减。各层片的碳密度与其Shannon-Wiener物种多样性指数之间没有显著的相关关系。     

基于IPSO-BP神经网络模型的山东省碳排放预测及生态经济分析

在低碳经济发展背景下,针对山东省碳排放数据更新迟缓、以往预测模型难以满足现实需求的问题,统计相关数据,根据政府间气候变化专门委员会(IPCC)推荐方法测算山东省2000—2017年碳排放量和排放强度,并借助脱钩分析、碳承载力和碳赤字探究碳排放的动态变化趋势;基于5项最重要的碳排放影响因素,建立改进的粒子群算法(IPSO...     

太行山东坡不同林龄杏树林碳储量及其分配特征

在生物量调查的基础上,对太行山东坡4、8、12年生和16年生杏树林生态系统碳储量及其分配特征进行了研究。结果表明:杏树各器官碳含量在447.3—488.1 g/kg;树干碳含量随林龄的增长而显著降低(P0.05),不同林龄间树根、树枝和树叶碳含量无显著差异;土壤层(0—100 cm)碳含量随林龄的增长而增大;随土层深度的增加而降低。林龄对杏树林乔木层、土壤层和生态系统碳储量均有显著影响。4、8、12年生和16年生杏树林生态系统碳储量分别为27.810、72.647、82.450 Mg/hm2和102.336Mg/hm2;土壤层碳储量占总碳储量的90.1%—99.6%,且主要集中于0—40 cm。乔木层碳储量分配随着林龄的增长而增加,土壤碳储量分配则减小。结果揭示了土壤层是杏树林生态系统的主要碳库;杏树人工林生态系统在生长过程中能显著地积累有机碳。研究结果可为经济林经营管理及碳汇功能评价提供参考。     

Perspective: Increasing blue carbon around Antarctica is an ecosystem service of considerable societal and economic value worth protecting

Precautionary conservation and cooperative global governance are needed to protect Antarctic blue carbon: the world's largest increasing natural form of carbon storage with high sequestration potential. As patterns of ice loss around Antarctica become more uniform, there is an underlying increase in carbon capture‐to‐storage‐to‐sequestration on the seafloor. The amount of carbon captured per unit area is increasing and the area available to blue carbon is also increasing. Carbon sequestration could further increase under moderate (+1°C) ocean warming, contrary to decreasing global blue carbon stocks elsewhere. For example, in warmer waters, mangroves and seagrasses are in decline and benthic organisms are close to their physiological limits, so a 1°C increase in water temperature could push them above their thermal tolerance (e.g. bleaching of coral reefs). In contrast, on the basis of past change and current research, we expect that Antarctic blue carbon could increase by orders of magnitude. The Antarctic seafloor is biophysically unique and the site of carbon sequestration, the benthos, faces less anthropogenic disturbance than any other ocean continental shelf environment. This isolation imparts both vulnerability to change, and an avenue to conserve one of the world's last biodiversity refuges. In economic terms, the value of Antarctic blue carbon is estimated at between £0.65 and £1.76 billion (~2.27 billion USD) for sequestered carbon in the benthos around the continental shelf. To balance biodiversity protection against society's economic objectives, this paper builds on a proposal incentivising protection by building a ‘non‐market framework’ via the 2015 Paris Agreement to the United Nations Framework Convention on Climate Change. This could be connected and coordinated through the Antarctic Treaty System to promote and motivate member states to value Antarctic blue carbon and maintain scientific integrity and conservation for the positive societal values ingrained in the Antarctic Treaty System.     

不同林龄格木人工林碳储量及其分配特征

在生物量调查的基础上,对广西7、29和32 a格木人工林生态系统碳储量及其分配特征进行了研究.结果表明: 格木各器官碳含量在509.0～572.4 g·kg^-1,大小顺序为:树干>树枝>树根>树皮>树叶;不同林龄间格木人工林的灌木层、草本层和凋落物层碳含量无显著差异;土壤层(0～100 cm)碳含量随土层深度的增加而降低,随林龄的增加而增大.7、29和32 a格木人工林乔木层碳储量分别为21.8、100.0和121.6 t·hm^-2,各器官碳储量大小顺序与碳含量一致;生态系统碳储量分别为132.6、220.2和242.6 t·hm^-2,乔木层和土壤层为主要碳库,占生态系统碳储量的97%以上.乔木层碳储量分配随着林龄的增加而增大,土壤碳储量分配则减小,而林龄对灌木层、草本层和凋落物层碳储量分配的影响无明显规律.     

Responses of Respiration to Increases in Carbon Dioxide Concentration and Temperature in Three Soybean Cultivars

The purpose of this experiment was to determine how respirationof soybeans may respond to potential increases in atmosphericcarbon dioxide concentration and growth temperature. Three cultivarsof soybeans (Glycine max L. Merr.), from maturity groups 00,IV, and VIII, were grown at 370, 555 and 740cm³m^-3carbon dioxideconcentrations at 20/15, 25/20, and 31/26°C day/night temperatures.Rates of carbon dioxide efflux in the dark were measured forwhole plants several times during exponential growth. Thesemeasurements were made at the night temperature and the carbondioxide concentration at which the plants were grown. For thelowest and highest temperature treatments, the short term responseof respiration rate to measurement at the three growth carbondioxide concentrations was also determined. Elemental analysisof the tissue was used to estimate the growth conversion efficiency.This was combined with the observed relative growth rates toestimate growth respiration. Maintenance respiration was estimatedas the difference between growth respiration and total respiration.Respiration rates were generally sensitive to short term changesin the measurement carbon dioxide concentration for plants grownat the lowest, but not the highest carbon dioxide concentration.At all temperatures, growth at elevated carbon dioxide concentrationsdecreased total respiration measured at the growth concentration,with no significant differences among cultivars. Total respirationincreased very little with increasing growth temperature, despitean increase in relative growth rate. Growth respiration wasnot affected by carbon dioxide treatment at any temperature,but increased with temperature because of the increase in relativegrowth rate. Values calculated for maintenance respiration decreasedwith increasing carbon dioxide concentration and also decreasedwith increasing temperature. Calculated values of maintenancerespiration were sometimes zero or negative at the warmer temperatures.This suggests that respiration rates measured in the dark maynot have reflected average 24-h rates of energy use. The resultsindicate that increasing atmospheric carbon dioxide concentrationmay reduce respiration in soybeans, and respiration may be insensitiveto climate warming. Glycine max L. (Merr.); carbon dioxide; respiration; temperature; climate change     

森林演替在南亚热带森林生态系统碳吸存中的作用

研究了鼎湖山南亚热带森林同一演替系列中3个不同演替阶段(马尾松针叶林、马尾松荷木混交林和季风常绿阔叶林)生态系统碳贮量和分配格局特征,并探讨了该地区森林演替过程中生态系统碳吸存潜力和速度。结果表明:(1)针叶林各组分碳素含量高于阔叶林对应组分的碳素含量(后者是前者的72.0%～94.5%)。两个森林植物碳素含量,不同层次比较,均为乔木层>灌木层>草本层,不同器官比较,以根或干最高。(2)乔木层生物量随森林演替进展而增加。针叶林、混交林和阔叶林乔木层生物量分别为:143.5t/hm2、270.1t/hm2和407.8t/hm2,其中大部分由干和皮组成(各器官占乔木层生物量的比例平均为:叶2.8%、枝19.3%、干和皮混合57.0%、根20.9%)。林下层生物量为4.23～14.10t/hm2,是乔木层的1.0%～9.8%,随森林演替进展而减少。(3)土壤容重随深度增加而增加,但随森林演替进展而减少。与土壤容重相反,土壤有机碳含量随深度增加而明显减少,但随森林演替进展而增加。(4)3种类型森林生态系统碳总贮量分别为135.8t/hm2、215.1t/hm2和259.7t/hm2。生态系统碳贮量在各组分的格局十分相似,植被、土壤和凋落物层所占比例均分别约为67.6%、30.2%和2.2%。与其它地带森林比较,鼎湖山保护区森林植被与土壤碳贮量之比和表层(0～20cm)的土壤碳占整个     

中国增汇型气候保护政策实施对经济的影响

系统地给出了中国实施增汇型CO2减排政策对宏观经济影响的模拟结果,所采用的模拟系统包括基于Pizer,Demeter,Zwaan工作发展的中国气候保护决策支持系统和中国经济可计算一般均衡(CGE)系统。研究结果表明,增汇型气候保护政策较其他单一的气候保护政策更有利于国家经济安全;虽然增汇型气候保护政策在短期内会对国家GDP产出造成影响,但从长远角度看,增汇型气候保护将带动经济的发展,是一项值得推广的减排政策。同时,发现中国实行每年增加4%的碳汇和实施4%能源替代以减少CO2排放控制率,辅助于0.2%的生产型CO2排放控制率,如果能够促进世界其它地区到2050年减排1990年的10%的CO,是一个合适的方案。     

南方双季稻田稻草还田的碳汇效应

利用长期稻草还田定位试验和短期不同稻草还田模式试验,研究稻草还田对南方双季稻田土壤固碳、甲烷排放和综合碳汇的影响.结果表明： 稻草还田能增加土壤有机碳,长期还田的耕层土壤碳汇年增长率为0.07 t C·hm^-2·a^-1,土壤有机碳的表观转化率随着稻草还田量的增加而减少.稻草还田导致稻田甲烷排放量显著增加,其中,NPK添加稻草（NPK+RS）处理早、晚稻期间甲烷排放通量比仅施NPK分别增加了75.0%和251.5%（P<0.01）.稻田甲烷排放随着稻草还田量的增加而增加,在水稻产量和耕作方式相近的条件下,稻草（茬）的甲烷表观转化率接近.综合土壤固碳和甲烷排放的稻田净碳汇,NPK+RS处理负碳汇效应显著,基本与其水稻生物固碳接近,比稻草不还田处理（NPK）增加158.3%;不同还田模式中,稻草覆盖免耕处理能显著减少甲烷排放,其净碳汇（负值）比高桩翻耕处理减少50.9%,有利于水稻高产稳产.     

增汇型气候保护的经济影响模拟分析

目前,将增汇作为气候保护的手段已在世界上引起了广泛重视。那么,增汇的经济可行性如何呢?我们认为,在经济发展的前提下,这个问题需要在宏观经济一般均衡的框架内进行讨论。针对这个问题,本文提出了对增汇型气候保护的经济影响进行评估的技术路线,建立了动态宏观经济分析模型进行模拟分析,得到了一些有意义的结论。