土壤易氧化有机碳与溶解性有机碳对荒漠草地沙漠化过程中土壤碳库变异的表征

以干旱、半干旱地区荒漠草地不同沙漠化阶段土壤为研究对象,研究不同沙漠化阶段土壤易氧化有机碳与溶解性有机碳含量和分配比例变异规律,分析不同沙漠化阶段土壤碳库指数变化,探讨荒漠草地沙漠化过程中土壤易氧化有机碳与溶解性有机碳对土壤碳库的表征作用。结果表明,随着荒漠草地沙漠化程度的加剧,易氧化有机碳含量表现出一定的波动性,但整体呈下降趋势,溶解性有机碳含量呈线性下降。易氧化有机碳和溶解性有机碳分配比例均在荒漠草地达到最大值,在半固定沙地达到最小值。利用易氧化有机碳含量计算的土壤碳库管理指数随荒漠草地沙漠化程度增加表现出先下降后上升趋势,利用溶解性有机碳含量计算的土壤碳库管理指数呈线性下降趋势。易氧化有机碳、溶解性有机碳含量与土壤有机碳均显著正相关,但溶解性有机碳的相关系数略高于易氧化有机碳。通过比较活度敏感指数和碳库管理指数敏感指数发现,荒漠草地逆向演替至固定沙地过程中,易氧化有机碳的各项敏感指数均高于溶解性有机碳。固定沙地演替至流动沙地过程中,溶解性有机碳的各项敏感指数均高于易氧化有机碳,表明易氧化有机碳能够较好地表征荒漠草地沙漠化前期土壤碳库变化,而荒漠草地沙漠化中期和后期利用溶解性有机碳表征效果更好。     

Black carbon estimation in French calcareous soils using chemo‐thermal oxidation method

We studied the black carbon (BC) content of ca. 405 samples from French topsoil and artificial soil and carbonate mixtures. Our protocol involved three main steps: (i) decarbonation by HCl, (ii) elimination of non‐pyrogenic organic carbon in a furnace at 375 °C, and (iii) quantification of residual carbon by CHN analysis. BC content increased for calcareous soils according to their carbonates content. Subsequent analyses confirmed the existence of a methodological artefact for BC determination only in calcareous soils. Decarbonation changes the thermal properties of organic matter, creating more recalcitrant carbon than in the initial sample. Higher CaCO₃ and organic carbon content results in a more pronounced artefact. The reversal of the first two steps of the chemo‐thermal oxidation method (i.e. thermal oxidation before soil decarbonation) eliminates this artefact. Overall, our results suggest that BC content may have been overestimated in a large number of studies on calcareous soils.     

保护性耕作对土壤团聚体、微生物及线虫群落的影响研究进展

保护性耕作具有良好的生态效益，有利于农业生态系统的可持续发展。本文对比分析了国内外有关常规耕作和保护性耕作措施对土壤团聚体、土壤有机碳、土壤微生物及土壤线虫影响的研究进展。结果表明：保护性耕作减少土壤大团聚体的破坏，降低团聚体周转速率，提高土壤结构的稳定性；保护性耕作提高表层土壤总有机碳及活性有机碳含量；保护性耕作可以提高耕层微生物生物量，尤其对真菌生物量影响显著；保护性耕作不同程度地提高了团聚体中微生物量和微生物多样性，但并未改变微生物在团聚体中的分布模式；保护性耕作可提高土壤线虫多度，提高原状土壤和土壤各粒级团聚体中线虫群落的成熟度指数和结构指数，但并未改变线虫总数、营养类群、功能团及生态指数在团聚体中的分布模式。针对目前国内外研究现状，展望了保护性耕作今后的研究重点，以期为因地制宜选取保护性耕作措施提供理论支持，推进我国农业可持续发展。     

秸秆还田对麦玉系统土壤有机碳稳定性的影响

为揭示不同秸秆还田量对华北小麦-玉米轮作系统土壤有机碳官能团结构及稳定性的影响,研究了秸秆还田5 a后土壤有机碳官能团结构、团聚体组成及有机碳含量、活性有机碳含量、土壤铁离子的变化。田间实验设置4个处理:秸秆不还田作为对照(CK)、秸秆1/3还田(S1)、秸秆2/3还田(S2)、秸秆全部还田(S3)。采用常规方法测定土壤理化性质、粒径、铁离子及土壤微生物量碳含量,13C核磁共振波谱技术(NMR)检测分析土壤有机碳官能团结构。结果表明:秸秆还田5 a后,土壤总有机碳(TOC)、2mm与2.00～0.25 mm团聚体有机碳、可溶性有机碳(DOC)、易氧化态碳(EOC)和微生物量碳(MBC)含量,均随还田量增加而逐渐增加,且不同处理增加量不同,与CK相比,S3处理显著增加了这些有机碳的含量(P0.05)。各处理土壤有机碳以烷基碳与烷氧基碳为主,其次是芳香碳与羰基碳,秸秆还田增加了烷氧基碳、羰基碳(易分解碳组分)含量,降低了烷基碳和芳香碳(难分解碳组分)含量,与CK相比,S3处理显著增加烷氧基碳含量(P0.05)而显著降低了芳香碳含量(P0.05)。与CK相比,S2、S3处理也显著降低了有机碳的芳香度、疏水碳/亲水碳、烷基碳/烷氧基碳比值(P0.05),而对脂族碳/芳香碳影响不明显。与CK相比,S3处理显著增加了2.00 mm团聚体组分,增加了2.00～0.25 mm组分,而降低了0.25～0.053 mm组分和显著降低了0.053 mm组分(P0.05)。秸秆还田对土壤游离铁、活性铁、螯合铁含量的影响不明显。有机碳官能团组成与土壤因子间的冗余分析表明土壤TOC、MBC含量、团聚体组分、铁离子的改变是导致不同处理间有机碳官能团结构存在差异的重要原因。综上所述,由于短期秸秆还田增加了活性有机碳含量、易分解有机碳组分,减少了难分解有机碳组分,降低了微团聚体物理保护作用,改变了微生物活性和铁离子络合作用,在一定程度上降低了土壤有机碳稳定性,可能导致麦玉复种系统土壤碳排放水平的增加。     

引入科研前沿对植物生理学教学方法的改进和效果分析

大学生普遍存在科研创新意识差、缺乏科研热情的现象.补充相关科研进展,将科研前沿引进课堂成为一种趋势,笔者对植物生理学光合作用这一章关于补充光合碳同化科研进展与否的教学实践结果进行对比分析,采用调查问卷的形式,围绕已讲授和未讲授光合碳同化适应性进化这一科研前沿进行调查,旨在实现学生对光合碳同化途径多元化发展进化的理解和深化,启发学生对固有知识的质疑和求解热情,达到提升科研兴趣和创新能力,实现精品课程培养满足国家和地方发展需要的高素质人才的目的.     

对我国LULUCF碳计量监测方法的探讨

围绕我国林业编制温室气体清单这一重要工作,介绍了IPCC关于LULUCF温室气体清单编制系列技术指南的技术要点和要求,阐明了我国林业温室气体清单编制工作的进展,提出了林业开展LULUCF碳监测工作未来面临的需求。同时,在分析美国、欧盟、加拿大等发达国家LULUCF温室气体清单编制做法和经验的基础上,提出了"在森林资源清查样地系统上构建"、"新布设LULUCF大样地系统"等2种开展LULUCF碳监测的思路,目的是为推动我国林业LULUCF碳监测达到国际先进水平提供建议。     

不同包膜肥用量对油菜碳氮代谢产物和产量的影响

为研究包膜肥在直播早熟油菜上的应用效果,采用田间小区试验,探究不同用量包膜肥对‘湘杂油1613’碳氮代谢和籽粒产量的影响。结果表明,施肥量相同条件下,施用包膜肥油菜碳氮代谢活跃,叶绿素含量(SPAD)升高,可溶性糖和游离氨基酸总量增加,含量差异不明显;单株有效分枝数和角果数明显增加,每角果粒数和千粒重小幅提高。施用包膜肥增产效果明显,包膜肥施肥量为1500 kg/hm~2时产量最高,达到2066.9 kg/hm~2。通过拟合建模,包膜肥用量为1611.0 kg/hm~2时,产量达到最高为2164.9 kg/hm~2;而普通肥的用量为1870.5 kg/hm~2时,最高产量为1904.8 kg/hm~2,包膜肥产量增加13.6%,同时用量减少13.9%。     

Environmental stress response limits microbial necromass contributions to soil organic carbon

The majority of dead organic material enters the soil carbon pool following initial incorporation into microbial biomass. The decomposition of microbial necromass carbon (C) is, therefore, an important process governing the balance between terrestrial and atmospheric C pools. We tested how abiotic stress (drought), biotic interactions (invertebrate grazing) and physical disturbance influence the biochemistry (C:N ratio and calcium oxalate production) of living fungal cells, and the subsequent stabilization of fungal-derived C after senescence. We traced the fate of ¹³C-labeled necromass from ‘stressed’ and ‘unstressed’ fungi into living soil microbes, dissolved organic carbon (DOC), total soil carbon and respired CO₂. All stressors stimulated the production of calcium oxalate crystals and enhanced the C:N ratios of living fungal mycelia, leading to the formation of ‘recalcitrant’ necromass. Although we were unable to detect consistent effects of stress on the mineralization rates of fungal necromass, a greater proportion of the non-stressed (labile) fungal necromass C was stabilised in soil. Our finding is consistent with the emerging understanding that recalcitrant material is entirely decomposed within soil, but incorporated less efficiently into living microbial biomass and, ultimately, into stable SOC.     

Short‐term releases of CO2 from newly mixed biochar and calcareous soil

The work aimed to quantify native organic C mobilized in one calcareous soil in the 21 days after addition of biochar at a range of large to very large applications. The experiment was carried out in unplanted microcosms, and CO₂ flux was used as a measure of net mineralization. A rapid methodological approach, which does not require ¹³C as a tracer, was used to assess any priming effects induced by the biochar. The amount of CO₂‐C mobilized was small relative to the amount of biochar C and proportional to the amount of the biochar added. The additional CO₂‐C was similar to the content of the water‐soluble organic carbon in the biochar added with each application. No interaction with native soil C, that is priming effect, was observed.     

Contribution of Different Organs to Grain Filling in Durum Wheat under Mediterranean Conditions I. Contribution of Post‐Anthesis Photosynthesis and Remobilization

Under Mediterranean conditions, drought affects cereals production principally through a limitation of grain filling. In this study, the respective role of post‐anthesis photosynthesis and carbon remobilization and the contribution of flag leaf, stem, chaff and awns to grain filling were evaluated under Mediterranean conditions in durum wheat (Triticum turgidum var. durum) cultivars. For the purpose, we examined the effects of shading and excision of different parts of the plant and compared carbon isotope discrimination (Δ) in dry matter of flag leaf, stem, chaff, awns and grain at maturity and in sap of stem, flag leaf, chaff and awns, this last measurement providing information on photosynthesis during a short period preceding sampling. Source–sink manipulations and isotopic imprints of different organs on final isotope composition of the grain confirmed the high contribution of both carbons assimilated by ears and remobilized from stems to grain filling, and the relatively low contribution of leaves to grain filling. Grain Δ was highly and significantly associated with grain yield across treatments, suggesting the utilization of this trait as an indicator of source–sink manipulations effects on grain yield. Chaff and awns Δ were better correlated with grain Δ than stem and leaf Δ, indicating that chaff were more involved in grain filling than other organs. Moreover, in chaff, sap Δ was highly significantly correlated with dry matter Δ. These results suggest the use of Δ for a rapid and non‐destructive estimation of the variation in the contribution of different organs to grain filling.