Question

epi lp studio四个调节旋钮的问题

新买了黑色的lp studio，把其中一个旋钮调到0，其他的10就没声音了，lp不是能独立调节拾音器的音量的吗，难道我的拾音器有问题？？？？高分求解……

Answer 1

les paul 四个旋钮 分别是前面两个音量旋钮volume 和两个音色旋钮tone 上下每两个音量和音色旋钮为一组~~上面一组管理前拾音器的音量和音色 下面一组管理后拾音器的音量和音色……而les paul并仅仅是用旋钮来控制拾音器工作的~~还有一个档位器~~当档位器的档位在上面的时候~~只有前拾音器工作~~这个时候~只有上面一组旋钮能够正常工作~~下面一组旋钮无论你怎么旋转都对声音产生不了什么作用~~同理~~当档位器在下面的时候~~只有后拾音器工作~~这个时候只有下面一组旋钮正常工作~~但是les paul并不是两个档位~~而是三个~~中间的前后拾音器共同工作的档位……在这个档位下 音量旋钮无法独立工作……当你关掉一个音量旋钮之后 另一个拾音器也不能发出声音了……所以要注意档位器和音量旋钮的正确使用……

Answer 2

New Zealand's Taranaki Basin, deep sandstone porosity evolution

Indonesia (Dereppe, etc., 1983) and South New Zealand (Newman foreign oil and gas exploration map 2Taranaki Basin wildcat stratigraphic column Maui-4 w 'Figure 3Taranaki Basin Maui a resolution of 4 exploration wells in four lump improved NMR spectrum, showing a signal dressed leather power range of solid and depth, 1988) 3km or 4km deep strata of coal spectrum, but the vast majority of coal from the coal mines of industrial value. Present work shows that the use of improved equipment than previous studies in more detail. In the coalification process, the loss of oxygen content in coal,abercrombie france, but not all of the functional groups are acidic substances, particularly alcohol and ether oxygen loss in the dehydration process; RCH - CH (OH) a R 'a R-CH = CH -R '+ H2O in Maul-4 wells in coal,franklin marshall femme, ethanol is caused by reasons for the low oxygen content (Table 1). In other polymer acid, the carboxylic acid can be released by decarboxylation of carbon dioxide: R-CO2H-RH + CO2Mokau coal as a low-rank coal (sub-bituminous) coal examples to study. It is the moisture content of 17, the carbon content (based on data analysis equipment) 73.8. In the decarboxylation, if all the oxygen is depleted, then the amount of acid per ton of wet coal (Table 1) can generate 150kg of COz. Of course, the low molecular weight organic acids can also release some of the functional groups. 200l006/ppm country 4Mokau increase the resolution of the NMR spectrum of coal country, showing a positive signal when the power range when the depth of 3.3km (Table 1), it seems that only about a quarter of the amount of acid to be preserved. Figure 3, the corresponding signal is weak, but time and time again. When the coal depth of 3.9km, the retention of the carboxylic acid content of the signal is not obvious (Table 1). Therefore, we conclude that the depth is greater than 3km above the coal, per ton of coal has released dozens of kilograms of COz. 7, No. 2 New Zealand Taranaki Basin, deep sandstone porosity evolution 199Dereppe, etc. (1983) in the upper stratum of peat, from the spectrum clearly on the form of oxygen found in the resolution of the aromatic carbon signals,birkenstock paris, the following in the depth of lkm coal spectrum is not too much of the acromion Crossey et al (1986) introduced the spectrum clearly demonstrates the existence of coal near the surface of the phenol and carboxyl groups, but in the deep coal 2756rn completely without these components. In contrast, our results clearly show the composition of aromatic carbon-oxygen until the depth of 4km. These functional groups include phenols, phenol ethers and heterocyclic structures. Discussion of mineral dissolution in sandstone. In particular,franklin marshall soldes, the dissolution of carbonate rock porosity of the Taranaki Basin produced hydrocarbons in the reservoir is very important, and hydrocarbons from the generation area of ??horizontal and vertical migration is also important. If New Zealand crude oil from the deep view is correct, then in the current below the depth of exploration, it may have hydrocarbon traps. Taranaki Basin, now widely distributed in dissolution pores mean by mature kerogen into CO and organic acids are rich in solvent, they migrated from the source rock reservoir, migration pathways, including cracks, residual porosity and the early formation of native secondary porosity and hydrocarbon solvent to generate a very short time interval between the release is important so as not to re-cement porosity. The NMR spectrum of coal sample shows western New Zealand, the world's other regions, it sets containing oxide material released from the coal, can be extended to at least 4km depth. South New Zealand GreatSouth basin also received similar data (Newman, 1988) the presence of CO-rich, may be formed directly from coal or the decarboxylation of organic acids formed. Acidic solvent close to the release of hydrocarbons present in the depth of the pore fluid, so the depth of the formation of secondary porosity have industrial value, and hydrocarbon generation prior to discharge to prevent re-cemented, at least to prevent carbonate cementation. * Theoretical and experimental data show that, before the formation of liquid hydrocarbons, oxygen-containing functional groups must be from one thousand to separate the kerogen molecules (Surdam and Crossey, 1985), but here the data for New Zealand's west hydrocarbons generated deep in the concept of providing evidence. Kerogen samples from the deepest of these molecular compounds are also described. Hydrocarbons is actually formed at higher temperatures, rather than early in the burial process and retained in the coal matrix generated in the cattle Booming (Tuha Petroleum Exploration and Development Research team) translated Journa / ofSoutheastAsianEarthSciences, Vo1.5, No . 1 4,1991 Zhangchao Fu School
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Answer 3

前面的旋钮是音量,后面两个是音色