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91.
92.
催化快速法测定CODCr是我国目前环境监测中普遍使用的最快速、简便、可靠的方法 ,该法的检测范围是 60~ 1 0 0 0mg/l,我们经过研究测出催化快速法的定量下限为 1 0mg/l,扩大了该法的应用范围。  相似文献   
93.
介绍了厌氧处理原理,并对厌氧处理低浓度废水的最新进展进行了较全面的综速,高效厌氧反应器及组合工艺为这一发展提供了可能。高效厌氧反应器中以膨胀颗粒污泥床(ECSB)反应器为首选。其结构及远行特性决定了它在处理低浓度虚水方面具有潜在的优势,但中国EC,SB的应用仅处于研究阶段,尚未有生产规模的EGSB;组合工艺对低浓度废水中污染物去除率极高,出水中COD、NH3-N、TP和SS浓度均可达到较高的排放标准,对生活污水、稀释后的工业有机废水等低浓度有机废水处理具有广阔的前景。  相似文献   
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The evaluation of biospheric role of the boreal forests in the accumulation of carbon is connected with the evaluation of organic matter (OM) pool in soils. The research sites were larch forests, they are situated on Nizhne-Tungusskoe Plateau. Larch forests of feather-moss and lichen types (110 and 380 years old) were formed on 'ochric podbur' soils. Litter stocks are 3.5–4.5 kg m− 2 with thickness 10–25 cm. Cryomezomorphic northern taiga soils contains 38–73 t (carbon) ha− 1. Pool of fast mineralized OM has average value 38.1 t (carbon) ha− 1, including 20.5 and 6.4 t (Carbon) ha− 1 of labile compounds on surface and in the soil, and 11.2 t (carbon) ha− 1 of mobile OM. Microbial mass reaches 1.78–3.47 t (carbon) ha− 1, its proportion is 3.6–4.9% of the total OM carbon. Zoomass of feather-moss larch forest is 0.20–0.61 * 10− 2, in lichen larch forest −0.01–0.07 * 10− 2 t (carbon) ha− 1. A pool of resistant to biological decomposition and bonded to mineral soil matrix OM is 17.7 t (carbon) ha− 1 and it varies from 18.6 to 29.0 in feather-moss larch forest, and from 6.4 to 17.0 t (carbon) ha− 1 in lichen larch forest. Two-years field experiment has been performed to determine transformation rates of various plant litter fractions and to clarify the role of soil biota in these processes. The results showed participation of all biota groups in the decomposition of plant residues caused weight loss of larch-needles and root mortmass. Isolation of organic matter from all-size invertebrate groups leads to some decrease of decomposition activity.  相似文献   
96.
Moesta  H.  Trappen  N. 《Die Naturwissenschaften》1970,57(1):38-39
The Science of Nature -  相似文献   
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Overestimates of black carbon in soils and sediments   总被引:2,自引:0,他引:2  
Several recent reports suggest that black carbon (BC), which broadly encompasses charcoal, soot, and other forms of pyrogenic carbon, may constitute a significant proportion of the refractory carbon in soil and sedimentary organic matter. BC is a sink for biospheric and atmospheric carbon dioxide, and is intimately tied to the biogeochemical cycling of both carbon and oxygen through its role in organic matter cycling. Additionally, BC may represent a large fraction of the missing carbon sink in global carbon accounting. Here, we demonstrate that documented measurements of BC may be the result of methodological artifacts, which inadvertently overestimate the amount of BC. We found that a widely used thermal oxidative method can create a residue that falls under the operational definition of BC in samples that are relatively BC-free. Moreover, during this procedure, labile organic matter constituents are condensed into pyrogenic carbon, implying that the labile components are present in lesser quantities. These methodological deficiencies are promoting overestimates in the amount of refractory carbon in soil and sedimentary organic matter and may endorse inaccuracies in the rates of carbon fluxes, the mean residence times of terrestrial carbon, and organic matter burial rates in oceanic environments.  相似文献   
100.
Chorionic villi obtained in the first trimester from a pregnancy at risk for α-mannosidosis were shown to have reduced α-mannosidase (EC 3.2.1.24) activity. The pregnancy was terminated and subsequent enzyme studies of the fetal tissues were consistent with the diagnosis of α-mannosidosis. Like the enzyme in the child's fibroblast, α-mannosidase of the chorionic villi from a pregnancy at risk for α-mannosidosis was activated by high substrate concentration and by Zn2 +, and displayed a Km value two-fold higher than normal. Our results confirm that chorionic villi can be used for early prenatal diagnosis of α-mannosidosis.  相似文献   
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