依兰县绿色食品发展现状与对策初探

针对依兰县绿色食品种植面积,种植基地建设,养殖基地建设,山产品采集基地建设,加工基地建设和销售基地建设及经济效益情况,提出了目前依兰县绿色食品开发已初步形成的标准体系框架并进行论述,评价分析了依兰县绿色食品产业的有利条件和制约困素,并提出发展的对策,使之逐步走向依兰县农业经济的主导地位.     

水中溶解氧快速测试管的研制

水中溶解氧不稳定，需要现场即时测定。本文旨在研究现场快速测定水中的溶解氧。本研究运用比色分析的朗伯——比尔定律和真空工艺设计，将复杂繁琐的实验室测试方法和操作程序有机的融合在测试管中。该测试管能快速、简便地测定水中的溶解氧。测定范围为0.01—12mg／1，检出限为0.0lmg／1。常规法测定时间需要3—5小时，而该测试管法仅需1—2分钟，分析成本也大为降低。     

YEP与数据通讯网络

ＹＥＰ采用了先进的计算机管理技术与电子邮件网络系统，到目前为止，省项目办和英国ＤＲＡ咨询专家与世界银行和涉及ＹＥＰ的各有关单位之间及时准确地进行了大量的数据传输工作，保证了ＹＥＰ工作的顺利进行。     

小麦发芽期锌的毒害作用和钙的去毒害作用研究

试验表明,较高浓度的Zn~(2+)对小麦种子的发芽和α-淀粉酶的活性有抑制作用.设置了胚芽鞘长/胚芽鞘粗和主胚根长/主胚根粗两项相对生长指标,发现:随Zn~(2+)处理浓度的提高,两项指标均逐渐下降.饱和CaCO_3和0.5％CaCl_2溶液对80ppmZn~(2+)处理过的小麦幼苗的毒害具一定解毒作用.对Ca~(2+)和pH条件与种子发芽时的形态建成和α-淀粉酶活性之间的关系进行了讨论.     

The effect of metapleural gland secretion on the growth of a mutualistic bacterium on the cuticle of leaf-cutting ants

In Acromyrmex octospinosus leaf-cutting ants the metapleural glands produce an array of antibiotic compounds that serve as a general defence against unwanted microbes on the cuticle. Leaf-cutting ants also grow mutualistic Pseudonocardiaceae bacteria on their cuticle that produce antibiotics controlling a microfungal parasite of their fungus gardens. Interaction between this bacterium and gland secretion therefore seems unavoidable. We document the typical development of bacterial growth on the cuticle of young major workers, show that growth starts a few days after eclosion, and that the maximal cover is reached after 2–3 weeks and gradually declines when workers mature. Experimental closure of the metapleural glands had no effect on the initial exponential growth phase of the bacterium, but significantly reduced the cover during the decline phase. The age-dependent abundance of the bacterium and its partial dependence on metapleural gland secretion support the hypothesis that the abundance of this mutualist is actively regulated.     

一种序批式生物膜反应器及其氧传递系数测定

介绍了一种序批式生物膜反应器 ,并求出了在给定的工艺条件下的氧传递系数。结果表明 :本反应器有较强的氧传递能力 ,能满足微生物的新陈代谢和降解有机污染物的需要     

煤气洗涤废水的处理研究

本研究对特难处理的煤气洗涤废水，采用混凝──电化学氧化处理，可获得良好的处理效果．其ＣＯＤ、油、酚分别由１０３２２ｍｇ／Ｌ、１５０００ｍｇ／Ｌ、１５７０ｍｇ／Ｌ降至２８９ｍｇ／Ｌ、１００ｍｇ／Ｌ、０．５ｍｇ／Ｌ．去除率分别为９７．２％，９３．３％，９９．９７％．     

Breccias of the Adnet Formation: indicators of a Mid-Liassic tectonic event in the Northern Calcareous Alps (Salzburg/Austria)

Stratigraphy, lithology and depositional structures of Liassic red limestone-breccias of the Adnet Formation, including the 'Adnet Scheck', were studied at several outcrops of the Northern Calcareous Alps (NCA) south-east of Salzburg. A four-fold lithostratigraphic division is proposed for the Adnet Formation of the Osterhorn Mountains: the hemipelagic Schmiedwirt (Sinemurian) and Kehlbach (Carixian) members are separated from the pelagic Saubach Member (Toarcian) by a layer of amalgamated breccias (Scheck Member, probably Domerian to early Toarcian). Several other breccia beds occur locally from the base of the Kehlbach Member up to the lower Saubach Member. Although the sediments overlying the Scheck Member breccias are of coeval age, the ages of the underlying strata are very different. This can be explained by submarine Liassic erosion during a period of resedimentation from the middle Carixian until the early Toarcian. At least 10–15?m of partly lithified sediments were eroded by gravity flows. The entire Kehlbach Member and up to two-thirds of the Schmiedwirt Member were removed at Adnet. The breccias originated from submarine debris flows. Repeated flows over a long period and the depositional setting exclude a triggering by sea-level fluctuations. Most probably they arose from tectonically triggered slumps and slides of superficial sediments. The 'Scheck' was initiated on the steep upper slope of the drowned Triassic Adnet reef and flowed to the north-east.The Pliensbachian to early Toarcian period of tectonic activity indicated by the breccias was the most important during the Liassic in the Osterhorn Mountains and other parts of the NCA. From the large-scale regional distribution of the breccias and in accord with published data, a roughly north-east trending strike-slip fault zone is proposed, crossing the NCA south of the Osterhorn block, with a peaking activity during the Pliensbachian to early Toarcian as the cause of the tectonic movements.     

Latest precambrian (Cadomian) zircon ages, Nd isotopic systematics and P-T evolution of granitoid orthogneisses of the Erzgebirge, Saxony and Czech Republic

Single zircons from two orthogneiss complexes, the Grey Gneiss and Red Gneiss, the lowermost tectonic units in the Erzgebirge, were dated. The grey Freiberg Gneiss is of igneous origin and has a ²⁰⁷Pb/²⁰⁶Pb emplacement age of 550±7 Ma. A quartz monzonite from Lauenstein contains idiomorphic zircons with a mean ²⁰⁷Pb/²⁰⁶Pb age of 555±7 Ma as well as xenocrysts ranging in age between 850 and 1910 Ma. Red gneisses from the central Erzgebirge contain complex zircon populations, including numerous xenocrysts up to 2464 Ma in age. The youngest, idiomorphic, zircons in all samples yielded uniform ²⁰⁷Pb/²⁰⁶Pb ages between 550±9 and 554±10 Ma. Nd isotopic data support the interpretation of crustal anatexis for the origin of both units. _Nd(t) values for the grey gneisses are –7.5 and –6.0 respectively, (mean crustal residence ages of 1.7–1.8 Ga). The red gneisses have a wider range in _Nd(t) values from –7.7 to –2.8 (T _DM ages of 1.4–1.8 Ga). The zircon ages document a distinct late Proterozoic phase of granitoid magmatism, similar in age to granitoids in the Lusatian block farther north-east. However, Palaeozoic deformation as well as medium pressure metamorphism ( 8 kbar/600–650° C) are identical in both gneiss units and distinguish these rocks from the Lusatian granitoids. The grey and red gneisses were overthrust by units with abundant high-pressure relicts and a contrasting P-T evolution. Zircon xenocryst and Nd model ages in the range 1000–1700 Ma are similar to those in granitoid rocks of Lusatia and the West-Sudetes, and document a pre-Cadomian basement in parts of east-central Europe that, chronologically, has similarities with the Sveconorwegian domain in the Baltic Shield.