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91.
K. G. Willis Malcolm Newson Sonja Boehmer‐Christiansen 《Journal of Environmental Planning and Management》1994,37(2):243-247
Cost Benefit Analysis of Environmental Change
Per‐Olov Johansson
Cambridge, Cambridge University Press, 1993, 232 pp., £13.95
Computerised Environmental Modelling: A Practical Introduction using Excel
J. Hardisty, D. M. Taylor & S. E. Metcalfe
Chichester, Wiley, 1993, 204 pp., £14.95
Keeping Pace with Science and Engineering: Case Studies in Environmental Regulation
Washington DC, US National Academy of Engineering, 1993
World Without End: Economics, Environment and Sustainable Development
D. W. Pearce & J. J. Warford
Oxford University Press, New York, 1993, 440 pp., £35.95 相似文献
92.
Recent drinking water regulations have lowered the disinfection by-product standards as well as added new disinfection by-products for regulation. Natural organic matter (NOM) plays a major role in the formation of undesirable organic by-products following disinfection/oxidation of drinking water. It is suspected that most precursors to disinfection by-products are humic, although nonhumic substances are also suspected of contributing to these by-products. Many of the disinfection by-products have adverse health effects in humans (i.e., carcinogenic or mutagenic effects). The primary chlorinated disinfection by-products of concern include trihalomethanes, haloacetic acids, and haloacetonitrile. Fluorescence spectroscopy was used to study humic and fulvic acids. The two fractions of humic substances, humic and fulvic acids, were characterized by a double-peak phenomena in an overlapping fluorescing region. Disinfection by-product formation potentials of humic and fulvic acids have been correlated with total organic carbon, UV absorbance at 254 nm, specific absorbance and fluorescence. River humic and fulvic acid was found to have the highest reactivity to disinfection by-product formation as compared to soil and peat humic and fulvic acid. Fluorescence spectroscopy has shown to be a rapid and predictive tool for disinfection by-products formation potential of humic and fulvic acids. 相似文献
93.
E. Lamla F. Boschke G. Traving G. Pfotzer H. Wolter W. Walcher H. D. Dahmen H. J. Queisser W. W. Klingbeil K. Beyermann O. Müller R. R. Ernst D. Reinen H. Muth W. Becker G. Wunsch G. I. Distler L. Jaenicke H. G. v. Schnering H. Werner F. Reiff H. Schimassek W. Höll H. K. Vasil W. F. Angermeier W. Ruppel J. C. Eccles G. Spiteller H. Oettel W. Vogell P. Brosche K. J. Hsü H. -U. Schmincke 《Die Naturwissenschaften》1975,62(3):143-143
94.
由于近二十年来全世界工业的快速发展 ,银的用途益发广泛 ,白银需求量迅猛增加 ,它不仅是我国紧缺的矿产资源 ,而且已成为世界市场上的走俏商品 ,全世界已连续九年需大于供 ,九年累计缺银 1 0亿盎司 ,并且缺口越来越大。专家们预测 :到 1 998年底全世界库存的银锭消耗殆尽。我国前几年有 1 / 2 -1 / 3的白银靠进口 ,1 997年还进口白银 1 55吨。因而 ,银价剧烈上扬 ,从 1 996年的 4美元 /盎司 ,涨到 1 998年 2月份的 7.81美元 /盎司。与白银相反 ,近两年黄金供远过于求 ,1 997年全世界多出 3 93吨 ,故金价急剧下跌 ,从 1 996年的 3 87.87美元 /盎司 ,降到 1 998年 6月份的 2 87.9美元/盎司。由于银需求量增大 ,加之有色金属工业的不景气 ,银产量不仅不能增长 ,而且反而下降。因而人们提出寻找能根据需要而生产的、具有独立开采价值的银矿床 ,即独立银矿床。全世界有三大巨型成矿带 ,我国有四大银成矿区。这些成矿区带的核心是火山 -岩浆活动带。银成矿区带都受巨型或区域深大断裂带控制 ,独立银矿床多产于区域深大断裂带旁侧的次级断层交汇处或附近。独立银矿床的直接围岩可以是火成岩、沉积岩和变质岩 ,但是它们位于火山岩浆活动带中 ,而且以火山岩为主。 相似文献
95.
96.
97.
E. A. Loupian A. A. Mazurov E. V. Flitman D. V. Ershov G. N. Korovin V. P. Novik N. A. Abushenko D. A. Altyntsev V. V. Koshelev S. A. Tashchilin A. V. Tatarnikov I. Csiszar A. I. Sukhinin E. I. Ponomarev S. V. Afonin V. V. Belov G. G. Matvienko T. Loboda 《Mitigation and Adaptation Strategies for Global Change》2006,11(1):113-145
98.
L. V. Mukhortova I. N. Bezkorovainaya 《Mitigation and Adaptation Strategies for Global Change》2006,11(1):191-202
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
99.
100.