广西西北部地区退化土地再造林项目人为净温室气体汇清除量预估

为了正确评估广西西北部地区退化土地再造林项目在应对气候变化中的作用,在全面收集项目区基础材料的基础上,结合大量的野外调查,估算了项目基准净温室气体汇清除量、实际净温室气体汇清除量以及泄漏,从而可较为精确地预估项目人为净温室气体汇清除量.预估结果,项目将在2008～2027年(20年)的首个计入期内产生1,405,447 t CO2 -e的tCER,年均70 272 t CO2-e.     

KH2PO4对设施油桃果实糖积累及代谢相关酶活性的影响

以设施栽培的艳光油桃为试材,研究了设施栽培条件下,喷施KH2PO4处理对油桃果实中糖积累和蔗糖代谢相关酶活性的影响。结果表明,幼果期喷施KH2PO4处理,果实葡萄糖和果糖含量明显增加,蔗糖含量没有明显变化,成熟期三种糖含量与对照均无明显差异;果实着色前KH2PO4处理显著增加了果实中蔗糖含量,但对葡萄糖和果糖含量无明显影响。幼果期和着色前喷施KH2PO4均显著提高了果实中蔗糖代谢酶活性。说明KH2PO4处理是通过全面提高果实中蔗糖代谢酶活性,起到提高库强作用,从而增加果实含糖量。     

Study on the Changes of the Amount of Microorganism and Microbial Biomass Carbon in Soil of Greenhouse Cropping

通过对四川省温江、双流两地不同设施种植年限土壤中微生物数量及其生物量碳的研究,结果表明,不同设施种植年限大棚土壤中的微生物数量是露地的1.63~3.50倍,且大棚土壤中好气性微生物总数随种植年限的增加有逐渐降低的趋势,三大微生物数量占微生物总数的比例中,细菌表现为随设施种植年限的增加而增加;放线菌和真菌表现为下降;露地土壤微生物多样性指数分别是设施年限为1a、2a和4a的大棚土壤的1.29倍、2.28倍和3.45倍,前者明显高于后者。随设施年限的增加,土壤微生物生物量碳、有机碳及微生物对有机碳的利用率都表现     

鸡粪沼液复合微生物有机肥在温室樱桃番茄上的应用效果研究

为了探讨鸡粪沼液复合微生物有机肥在樱桃番茄上的田间应用效果,在滴灌施肥的条件下,设置化肥和液体复合微生物有机肥两个处理进行对比应用,结果表明施用液体复合微生物有机肥的处理其单果重可提高39.69%,含糖量可提高11.94%,茎粗可提高8.76%,Vc含量可提高5.72%,产量可提高30.95%,节约成本1.32%,可有效促进作物生长,提高果实着色均匀度,提高作物抗病性。同时,土壤速效氮提高6.87%,土壤速效磷46.23%,土壤速效钾提高16.86%,有机质含量提高12.64%,为作物提供了良好的生长环境。说明液体复合微生物有机肥对作物产量、品质以及土壤改良均有显著的提升作用,具有一定的应用前景。     

地源热泵技术在中国温室设施中的应用探讨

当前在中国温室设施中应用和推广地源热泵技术尚存在诸多不利因素,大大限制了该项技术在设施农业领域中的发展。为探寻合理的解决途径,对地源热泵空调系统的关键技术和其在中国的发展概况进行了相关的阐述和分析,并以中国农业大学上庄实验站已经建成使用的地下水式温室地源热泵空调系统为实例,介绍该系统的组成、工作流程、性能参数和使用情况,探讨温室地源热泵空调系统在推广和使用中可能出现的投资较高,长时间运行性能不稳定等问题,分析其原因并提出相应的对策建议。     

日光节能温室油桃早果丰产栽培试验

就日光节能温室油桃早果丰产栽培技术从大苗定植、扣时间的确定、全园覆膜、多效唑控冠、蜜蜂与人工辅助授粉等几个方面进行了试验和探讨     

日光温室间作新模式对环境因子及菇菜生长的影响

采用反遮光内拱棚模式,在日光温室内进行菇菜间作,研究对环境因子及菇菜生长的影响。结果表明:反遮光内拱棚日均温度15.5℃,最高22℃,最低12℃;相对湿度平均96.7%,最高99%,最低90%;光照强度最高为0.5klx;CO2平均浓度为828μL·L-1,最高为1000μL·L-1,最低为630μL·L-1,完全满足金针菇生长需求。通过斜拉秧措施,极大提高了黄瓜窄行光照强度,提高了保护地栽培效益。     

墙体材料及其组合对日光温室墙体保温性能的影响

利用热反应系数法和日光温室热环境的数学模型模拟分析了日光温室墙体得热量、墙体温度以及室内气温,比较了墙体材料的不同组合对保温性能的影响。结果表明,对不同厚度砖墙聚苯板隔热材料的厚度以0.10m为宜;相同厚度隔热材料在砖墙厚度较薄时保温效果优于较厚的砖墙;砖墙厚度较薄时材料的排列秩序对保温影响较明显。     

地热——太阳能干燥室温室兼用装置研究

地热——太阳能干燥室温室兼用装置的热源是低温地热能(60～70℃地热水)和太阳能。该装置夏季用于干燥,冬季用于温室栽培,使一套装置多种用途,全年使用。该装置通过强制通风和自然通风的选择,地热水流量、新风风量和回风风量的调节,在干燥过程中实现了低温地热能和太阳能的合理匹配与互补,满足了不同工况的要求。     

Fluxes of CO2, CH4 and N2O from drained organic soils in deciduous forests

We examined net greenhouse gas exchange at the soil surface in deciduous forests on soils with high organic contents. Fluxes of CO₂, CH₄ and N₂O were measured using dark static chambers for two consecutive years in three different forest types; (i) a drained and medium productivity site dominated by birch, (ii) a drained and highly productive site dominated by alder and (iii) an undrained and highly productive site dominated by alder. Although the drained sites had shallow mean groundwater tables (15 and 18 cm, respectively) their average annual rates of forest floor CO₂ release were almost twice as high compared to the undrained site (1.9±0.4 and 1.7±0.3, compared to 1.0±0.2 kg CO₂ m⁻² yr⁻¹). The average annual CH₄ emission was almost 10 times larger at the undrained site (7.6±3.1 compared to 0.9±0.5 g CH₄ m⁻² yr⁻¹ for the two drained sites). The average annual N₂O emissions at the undrained site (0.1±0.05 g N₂O m⁻² yr⁻¹) were lower than at the drained sites, and the emissions were almost five times higher at the drained alder site than at the drained birch site (0.9±0.35 compared to 0.2±0.11 g N₂O m⁻² yr⁻¹). The temporal variation in forest floor CO₂ release could be explained to a large extent by differences in groundwater table and air temperature, but little of the variation in the CH₄ and N₂O fluxes could be explained by these variables. The measured soil variables were only significant to explain for the within-site spatial variation in CH₄ and N₂O fluxes at the undrained swamp, and dark forest floor CO₂ release was not explained by these variables at any site. The between-site spatial variation was attributed to variations in drainage, groundwater level position, productivity and tree species for all three gases. The results indicate that N₂O emissions are of greater importance for the net greenhouse gas exchange at deciduous drained forest sites than at coniferous drained forest sites.