新疆猪毛菜属17种C_4植物叶片和子叶的解剖结构研究

通过对藜科猪毛菜属17种C4植物的叶片和子叶的解剖学研究,共得到2种叶片的解剖结构类型,Salsoloid具有皮下组织型(SALS+H型)和Salsoloid不具有皮下组织型(SALS-H型);4种子叶的解剖结构类型分别是C3-异面叶型(C3-DV型)、Atriplicoid且具有皮下组织型(ATR+H型)、SALS+H型和SALS-H型。同一种植物子叶和叶片的解剖结构类型并不完全一致,分为2大类。一类是子叶和叶片都是C4型解剖结构,包括叶片SALS+H型/子叶ATR+H型、叶片SALS+H型/子叶SALS+H型和叶片SALS-H型/子叶SALS-H型;另一类是叶片具有C4型解剖结构,子叶具有C3型解剖结构,包括叶片SALS+H型/子叶C3-DV型和叶片SALS-H型/子叶C3-DV型。同组植物子叶和叶片的解剖结构类型具有一定的规律性,不同组之间植物光合器官的解剖结构类型存在较大的差异,这些差异性与植物生活型、地理分布没有关系。     

冬季种养结合对稻田土壤微生物量及有效碳氮库的影响

以双季稻冬闲田种植绿肥与养鸡结合的新型种养制度为平台,通过冬季绿肥和鸡粪还田,减少水稻生育期化肥用量,探讨“冬季绿肥-双季稻”轮作种植制度和“冬季种养结合-双季稻”种养制度下对稻田土壤微生物碳、氮和可溶性有机碳、氮的影响。试验包括5个处理,分别为冬闲(F)、冬季种植黑麦草(R)、冬季种植紫云英(M)、冬季种植黑麦草与养鸡结合(RC)以及冬季种植紫云英与养鸡结合(MC)。结果表明,在整个试验的动态过程中,微生物量碳、氮及可溶性有机碳、氮含量高低总体趋势表现为绿肥养鸡>绿肥>冬闲,各处理间差异显著(P<0.05);“冬季种养结合-双季稻”种养制度能显著提高土壤微生物量碳、氮和可溶性有机碳、氮。各处理微生物量碳、氮和可溶性有机氮在3月24日达到最大值,RC、MC、R和M处理微生物量碳最大值分别为492.22,464.91,432.34和435.48 mg/kg;微生物量氮的最大值分别为118.20,101.03,70.13和85.46 mg/kg;可溶性有机氮的最大值分别为1001.47,926.21,832.80和870.75 mg/kg;可溶性有机碳在早稻苗期达到最大值,RC、MC、R和M最大值分别为278.95,266.40,246.13和249.84 mg/kg。微生物量碳含量的高峰在早稻移栽初期、晚稻孕穗期和灌浆期,微生物量氮的高峰出现在早稻分蘖期、齐穗灌浆期和晚稻孕穗期,可溶性有机碳在稻田养鸡及成鸡出栏后较高。与冬闲田种植绿肥和休闲相比,冬闲稻田种植绿肥结合养鸡对增加微生物生物量的贡献更大,并显著提高土壤的可溶性有机碳氮,间接反映了种养制度能提高土壤有机碳、氮的矿化速率和土壤的活性有机碳氮以及满足水稻生长期间自身养分需求。     

冬季作物对水稻生育期土壤微生物量碳、氮的影响

选取我国南方4种冬季作物黑麦草、紫云英、油菜、马铃薯,以冬闲田作对照,对水稻生育期土壤微生物量碳（SMBC）和土壤微生物量氮（SMBN）的短期内动态变化进行了研究。结果表明,早稻田翻耕前,冬季作物处理土壤SMBC和SMBN与冬闲田存在显著差异(P0.05),黑麦草处理SMBC为398.5 mg/kg,显著高于其他作物;紫云英处理SMBN最高,为97.8 mg/kg。在早稻整个生育期,黑麦草处理SMBC显著高于其他处理,晚稻生长过程中各处理无显著差异。冬季作物对稻田土壤微生物商(MQ)的影响,随着水稻生长发育进程有不同程度的变化,黑麦草处理在早稻整个生育期高于冬闲田。     

Accumulation and composition of total organic carbon in reclaimed coal mine lands

Reclaimed coal mine lands have the potential to sequester atmospheric carbon (C); however, limited information exists for the western USA coalfields. This study was carried out on two chronosequences (BA‐C₃ grasses and DJ‐shrubs) of reclaimed sites at two surface coal mines to determine the effects of vegetation, soil texture, and lignin content on soil total organic carbon (TOC) accumulations. In the BA chronosequence, TOC increased over 26 years at an average rate of 0·52 Mg C ha⁻¹ yr⁻¹ in the 0–30 cm depth and was significantly correlated with clay content. Comparison between < 1 and 16‐year‐old stockpile soils indicated TOC content did not differ significantly. In the DJ chronosequence, TOC content in the 0–30 cm depth declined from 31·3 Mg ha⁻¹ in 5‐year‐old soils to 23·4 Mg ha⁻¹ in 16‐year‐old soils. The C:N ratios suggested that some (up to 2·0 per cent) of the TOC was potentially derived from coal particles in these reclaimed soils. Soil total N (TN) contents followed a similar trend as TOC with TOC and TN concentrations strongly correlated. Lignin contents in TOC of all reclaimed soils and topsoil stockpiles (TSs) were higher than that of nearby undisturbed soils, indicating the recalcitrant nature of TOC in reclaimed soils and/or possibly the slow recovery of lignin degrading organism. Results indicated that TOC accumulations in DJ were largely controlled by its composition, particular lignin content. In BA sites TOC accumulation was strongly influenced by both clay and lignin contents. Copyright © 2008 John Wiley & Sons, Ltd.     

Abiotic soil properties and the occurrence of Rhizoctonia crown and root rot in sugar beet

Since 1993, Rhizoctonia crown and root rot (Rhizoctonia solani AG 2–2 IIIB) has represented an increasing problem for sugar beet production in Germany. Up to now, the outbreak of the infection and the spread of the disease within a field cannot be predicted and effective countermeasures are not available. Although little is known about the living conditions of R. solani in soils, abiotic soil properties are likely to influence the disease occurrence. Investigations were carried out based on 60 pairwise comparisons, each consisting of a disease‐affected and an adjacent nonaffected patch on farmers' fields in 2002 and 2003. Soil samples from the top soil layer (0–30 cm) were collected before harvest, and eight of the most frequently mentioned soil properties potentially influencing Rhizoctonia crown and root rot infection were examined: bulk density, texture, carbonate carbon, potassium, phosphorus, organic carbon, total nitrogen, and pH. The occurrence of the disease was significantly related to the soil C : N ratio, indicating the influence of soil organic matter on the disease occurrence. Examinations of soil thin sections showed that organic‐matter particles in the soil serve as a substrate for R. solani. All other soil physical and chemical properties examined did not differ between the disease‐affected and nonaffected patches and seem to be of minor importance.     

Three‐source partitioning of CO2 efflux from maize field soil by 13C natural abundance

A natural‐¹³C‐labeling approach—formerly observed under controlled conditions—was tested in the field to partition total soil CO₂ efflux into root respiration, rhizomicrobial respiration, and soil organic matter (SOM) decomposition. Different results were expected in the field due to different climate, site, and microbial properties in contrast to the laboratory. Within this isotopic method, maize was planted on soil with C₃‐vegetation history and the total CO₂ efflux from soil was subdivided by isotopic mass balance. The C₄‐derived C in soil microbial biomass was also determined. Additionally, in a root‐exclusion approach, root‐ and SOM‐derived CO₂ were determined by the total CO₂ effluxes from maize (Zea mays L.) and bare‐fallow plots. In both approaches, maize‐derived CO₂ contributed 22% to 35% to the total CO₂ efflux during the growth period, which was comparable to other field studies. In our laboratory study, this CO₂ fraction was tripled due to different climate, soil, and sampling conditions. In the natural‐¹³C‐labeling approach, rhizomicrobial respiration was low compared to other studies, which was related to a low amount of C₄‐derived microbial biomass. At the end of the growth period, however, 64% root respiration and 36% rhizomicrobial respiration in relation to total root‐derived CO₂ were calculated when considering high isotopic fractionations between SOM, microbial biomass, and CO₂. This relationship was closer to the 50% : 50% partitioning described in the literature than without fractionation (23% root respiration, 77% rhizomicrobial respiration). Fractionation processes of ¹³C must be taken into account when calculating CO₂ partitioning in soil. Both methods—natural ¹³C labeling and root exclusion—showed the same partitioning results when ¹³C isotopic fractionation during microbial respiration was considered and may therefore be used to separate plant‐ and SOM‐derived CO₂ sources.     

不同C/N对堆肥腐殖酸的影响

以鸡粪、稻草为原料,采用条垛式高温堆肥,研究C/N对堆肥腐殖酸的影响.结果表明,C/N对富里酸生成无显著影响;C/N在20～35间有利于总腐殖酸和水溶性腐殖酸的形成;C/N在20～30间有利于游离腐殖酸和胡敏酸的生成;C/N为30,堆肥腐熟后总腐殖酸生成量最多.     

全新世早期黄河上游积石峡大型滑坡堵江事件研究

普遍认为黄河上游积石峡地区厚约30m的纹泥沉积是由于大型滑坡堵江形成的,然而,滑坡堵江时代以及堵江形成的堰塞湖纹泥沉积历时仍有争议。为了探讨研究区大型滑坡堵江时代及纹泥沉积历程,文中在纹泥底部和顶部各采集1个样品进行14C年代测定。纹泥底部样品的14C年代为9016±425 cal a B.P.,纹泥顶部样品的14C年代为7984±334 cal a B.P.。研究结果表明:黄河上游积石峡地区曾在全新世早期距今约9ka左右发生过大型堵江事件,纹泥沉积的沉积历程约为1ka,这与前人利用纹泥层厚度估算的沉积历程相吻合。该研究可为下游地区第四纪时期文明演化的研究提供一些新的参考。     

Decomposition of Medicago sativa Debris Incubated at Different Depths under Mediterranean Climate

Reports on the dynamics of carbon and nitrogen at different depths in soil profiles usually describe a higher mineralization of both at upper horizons. Nevertheless, under Mediterranean climate, upper soil horizons are strongly affected by drought, especially in summer, and may offer pedoclimatic conditions less favorable to microbial activity than deep soil layers. Therefore, decomposition could be slower in the upper soil layers. To test this hypothesis, mixtures of Medicago sativa ground plants and soil material were incubated in the field, at 5, 20, and 40 cm depth, in nylon mesh bags. Mineralization of carbon and nitrogen was studied for two years. At 5 cm, mineralization of both elements was lower, and no differences were found between 20 and 40 cm. After two years of field incubation, the remaining carbon (as a percentage of the initial content) was 27.95 % +/- 0.88 at 5 cm depth, 19.87% +/- 0.77 at 20 cm, and 18.78 % +/- 1.19 at 40 cm. Mineralization of nitrogen exceeded that of carbon. After two years of field incubation, the remaining nitrogen (as a percentage of the initial content) was 17.62% +/- 3.06 at 5 cm depth, 12.17% +/- 0.94 at 20 cm, and 11.26% +/- 0.99 at 40 cm. The biodegradation rate in upper layers was lower for all biochemical fractions (water-soluble compounds, lipids, polysaccharides, lignin). This contrasts with the usual findings on this topic, but is consistent with our previous results with forest litter samples. Mineralization clearly followed double-exponential kinetics, with a labile and a recalcitrant pool of both carbon and nitrogen. The labile pool of carbon accounted for about 50% of the total initial carbon, whereas that of nitrogen accounted for about 60%. No clear effect of depth on the proportion between the labile and the recalcitrant pool was observed, neither for carbon nor for nitrogen. It was not possible to identify both pools with the biochemical fractions, suggesting that these pools should be interpreted in physical terms (unprotected vs. protected ). No direct effect of depth on the global retention of N was detected.     

合成气合成低碳醇热力学及试验研究

为了解决液体燃料缺乏以及农业废弃物处置的问题,该文分析了合成低碳醇的重要性,提供了一条解决农业废弃物的方法,并通过热力学分析指导低碳醇的合成.文中使用平衡常数法对合成气合成低碳醇进行热力学分析计算,并验证了计算结果符合理论分析的趋势,得到降低温度、提高压力有利于CO的转化和醇类的生成,以及不同H2/CO摩尔比的情况下C...