长江经济带林地和其他生物质碳储量及碳汇量研究

以全国林业应对气候变化碳汇计量监测体系建设结果数据为基础，应用森林碳库专项调查建立的碳计量模型和参数，结合历次森林资源清查成果等数据，估算了2020年长江经济带林地和其他生物质碳储量和碳汇量。研究表明：（1）2020年长江经济带林地碳储量24543.58 Tg C （其中森林植被碳储量为4372.85Tg C），散生木和四旁树等其他生物质碳储量329.59 Tg C。2020年长江经济带林地碳汇量81.81 Tg C/a （300.26Tg CO₂/a）、散生木和四旁树等其他生物质碳汇量6.60 Tg C/a （24.21 Tg CO₂/a）。无论是林地和其他生物质碳储量、碳汇量、还是森林植被碳储量，乔木林地所占比例最大（69%-85%）；长江经济带11个省市中，云南省最大，上海市最小；林地碳储量中土壤有机质碳库贡献最大（81.46%），林地碳汇量中生物量碳库贡献最大（90.99%）；林地碳汇量中"一直为林地的土地"产生碳汇量贡献最大（71.74%），其中一直为乔木林的土地产生的碳汇量占69.89%；（2）阐述了长江防护林工程、天然林资源保护工程、珠江防护林工程和沿海防护林工程4大重点生态工程对长江经济带碳储量和碳汇量的贡献，长江防护林工程贡献率最大（81%-83%），其次是天然林资源保护工程（32%-38%），珠江防护林工程和沿海防护林工程影响较小。分析了人工造林、中幼林抚育、次生林和低效林改造、退化林修复等生态保护修复措施对长江经济带碳储量和碳汇量的贡献，并提出了碳中和愿景下森林固碳增汇的有效途径。     

接种丛枝菌根真菌对云南石漠化土壤呼吸的影响

为探明"丛枝菌根（Arbuscular mycorrhiza，AM）真菌-植物-土壤"耦合作用对石漠化土壤呼吸季节动态的影响，采用LI-6400-09土壤呼吸室和便携式光合作用测量系统，对圆柏（Sabina chinensis）接种摩西斗管囊霉（Funneliformis mosseae，FM）、根内根孢囊霉（Rhizophagus intraradices，RI）2种AM菌种处理下土壤呼吸季节动态进行野外连续定位观测，并探究AM真菌接种处理下石漠化土壤呼吸速率与植物生长、土壤理化性质之间的关系。结果表明：（1）相较于对照，接种AM真菌对石漠化生境土壤呼吸季节动态产生了显著影响（P<0.01）。AM真菌处理具有较高的土壤呼吸季节变化幅度，即根内根孢囊霉处理土壤呼吸速率（1.55-9.10 μmol m^-2 s^-1）显著高于摩西斗管囊霉（1.62-8.29 μmol m^-2 s^-1）和对照（1.23-4.46 μmol m^-2 s^-1）；（2） AM真菌接种处理下土壤温湿度变化对土壤呼吸的影响显著大于对照，即土壤温度与水分对土壤呼吸的平均解释量大小顺序为：RI （44.84%；52.35%）>FM （17.18%；41.65%）>CK （2.66%；16.55%）；（3）2种菌种处理下土壤呼吸速率均与土壤有机质、硝态氮、全氮、速效钾、树高、胸径及根系生物量呈显著或极显著正相关（P<0.01或0.05），而与pH呈极显著负相关（P<0.01），但对照处理土壤呼吸速率除与pH呈显著负相关（P<0.05）外，与其它土壤理化指标相关性不显著；（4）土壤温度和水分、硝态氮、铵态氮、有机质、易氧化有机碳、速效钾、全氮及全磷对土壤呼吸变化的贡献最大，而胸径、树高、有效磷、微生物生物量、根系生物量及pH的影响次之。因此，"AM真菌-寄主植物-土壤"相互作用对石漠化生境土壤呼吸季节动态的影响，主要取决于不同AM真菌接种处理对土壤微气候（如含水量）、碳素（有机质、易氧化有机碳）、无机氮库（铵态氮、硝态氮）、根系生物量及磷钾养分可利用性的调控。     

Warming increases soil carbon input in a Sibiraea angustata-dominated alpine shrub ecosystem

Plant-derived carbon (C) inputs via foliar litter, root litter and root exudates are key drivers of soil organic C stocks. However, the responses of these three input pathways to climate warming have rarely been studied in alpine shrublands. By employing a 3-year warming experiment (increased by 1.3 °C), we investigated the effects of warming on the relative C contributions from foliar litter, root litter and root exudates from Sibiraea angustata, a dominant shrub species in an alpine shrubland on the eastern Qinghai-Tibetan Plateau. The soil organic C inputs from foliar litter, root litter and root exudates were 77.45, 90.58 and 26.94 g C m⁻², respectively. Warming only slightly increased the soil organic C inputs from foliar litter and root litter by 8.04 and 11.13 g C m⁻², but significantly increased the root exudate C input by 15.40 g C m⁻². Warming significantly increased the relative C contributions of root exudates to total C inputs by 4.6% but slightly decreased those of foliar litter and root litter by 2.5% and 2.1%, respectively. Our results highlight that climate warming may stimulate plant-derived C inputs into soils mainly through root exudates rather than litter in alpine shrublands on the Qinghai-Tibetan Plateau.     

中国航空碳排放及其效率时空演化特征分析

航空碳排放不仅影响空气质量且可造成温室效应。中国正处于从民航大国向民航强国迈进的关键时期，提高航空碳排放效率是行之有效的航空碳减排手段。运用可拓展随机性环境影响评估模型(STIRPAT)对中国2004—2019年航空碳排放总量的时空演变特征进行分析，以探明不同尺度区域航空碳排放的空间差异与空间关联表现；运用基于非期望产出的超效率松弛变量模型(SBM)和标准差椭圆分析法(SDE)对中国航空碳排放效率的时空分布与格局演化过程进行判定，以分析各省域航空碳排放效率的差异，并给出有效的航空碳减排方略。研究发现：2004—2019年，中国航空碳排放总量持续增长，航空碳排放增长率和航空碳排放强度均呈波动下降趋势；四大经济区航空碳排放总量分布总体表现为“东部>西部>中部>东北”的格局，东部仍是中国航空碳排放的主要区域；高碳排放区较分散，还未形成省域之间连片的碳排放高值区。2004—2019年，中国航空碳排放效率总体呈现“M”型波动上升趋势，各省域航空碳排放效率均不同程度的提高，但主要以低效率区、中效率区为主；各省域之间的航空碳排放效率差异性经历了逐渐减小到逐步增大的过程，但总体航空碳...     

Forest floor photosynthesis and respiration in a drained peatland forest in southern Finland

Background: Although forest floor forms a large biomass pool in forested peatlands, little is known about its role in ecosystem carbon (C) dynamics.

Aim: We aimed to quantify forest floor photosynthesis (P _FF) and respiration (R _FF) as a part of overall C dynamics in a drained peatland forest in southern Finland.

Methods: We measured net forest floor CO₂ exchange with closed chambers and reconstructed seasonal CO₂ exchange in the prevailing plant communities.

Results: The vegetation was a mosaic of plant communities that differed in CO₂ exchange dynamics. The reconstructed growing season P _FF was highest in the Sphagnum community and lowest in the feather moss communities. On the contrary, R _FF was highest in the feather moss communities and lowest in the Sphagnum community. CO₂ assimilated by the forest floor was 20–30% of the total CO₂ assimilated by the forest. The forest floor was a net CO₂ source to the atmosphere, because respiration from ground vegetation, tree roots and decomposition of soil organic matter exceeded the photosynthesis of ground vegetation.

Conclusions: Tree stand dominates C fluxes in drained peatland forests. However, forest floor vegetation can have a noticeable role in the C cycle of peatlands drained for forestry. Similarly to natural mires, Sphagnum moss-dominated communities were the most efficient assimilators of C.     

祁连山南麓高寒湿地生态系统呼吸季节、年际动态及影响因素

由于青藏高原高海拔、低温的特殊环境，使得生态系统呼吸(RE)对气候变化的响应极其敏感，然而对高寒湿地生态系统长时间尺度上的RE动态特征及驱动机制的研究相对薄弱。以青藏高原东北部高寒湿地为研究对象，分析了基于涡度相关系统观测的高寒湿地2004—2016年的CO₂通量排放动态及影响机制，对预测高寒湿地碳平衡对未来气候变化的响应具有重要意义。结果表明：高寒湿地在2004—2016年的月平均RE表现为单峰变化趋势，在8月达到峰值；年RE表现为逐年升高的趋势(P<0.05),年RE均值为(608.9±65.6) g C m^-2 a^-1;生长季RE约是非生长季RE的2.7倍，线性回归分析表明生长季RE(r~2=0.66,P=0.001)、非生长季RE(r~2=0.47,P=0.01)与全年RE呈极显著正相关。在月尺度上，分类回归树分析和线性回归分析表明土壤温度是月RE的最主要控制因素，暗示高寒湿地的土壤呼吸对整个生态系统的碳排放至关重要。在年际尺度上，生长季积温与生长季RE呈显著正相关(P<0.05),而生长季降水(PP...     

Cytoplasmic Acidification May Occur in High-Pressure Carbon Dioxide-Treated Escherichia coli K12

While studying the mechanism by which high-pressure carbon dioxide treatment (HCT) inactivates bacteria, we found that the efficiency of DNA recovery via phenol extraction was extraordinarily low from E. coli K12 cells that had been subjected to HCT. DAPI staining of the treated cells, however, revealed that nuclear DNA was present. Most DNA from the cells subjected to HCT was probably caught in the denatured protein layer during phenol extraction. The efficiency of DNA recovery from proteinase-treated crude extracts from cells subjected to HCT was high. Crude extracts of E. coli K12 cells that had not undergone HCT were intentionally acidified with acetic acid to pH 5.2 to cause acidic coagulation of cytoplasmic proteins. The efficiency of DNA recovery from the acidified extracts was low. These results suggest that in cells subjected to HCT, cytoplasmic pH is reduced to around pH 5.2, and that nuclear DNA becomes entangled in coagulated cytoplasmic proteins. Acidification of the cytoplasm might be the primary mechanism by which HCT inactivates bacteria.     

The effect of soil aggregate size on early growth and shoot-root ratio of maize (Zea mays L.)

Shoot dry mass and leaf area of 16-d old maize plants decreased as soil aggregate size in greenhouse pots increased in diameter from 0.075–0.5 to 4–8 mm. Root length was also much greater on the finer aggregate beds, due primarily to increased growth of second-order laterals. In a subsequent experiment in which shoot dry matter again decreased with increasing aggregate size, it was found that a similar change in root morphology as noted in experiment I resulted in increased root dry mass as aggregate size increased. The associated change in shoot-root ratio was significant eight days after emergence. This change was due to a change in allocation of fixed carbon rather than allocation of seed reserves. Neither transpiration rate per unit leaf area, nor net assimilation rate were affected by aggregate size. Likewise nutrition could not account for the differences in shoot or root growth.