Does Tianlong Babu 3 make money by mining
preparation:
1. There should be 2 ~ 3 warehouses, and the cost is 5 ~ 10J
2. Learn mining and medicine, the price of grade 5 mine and medicine is 3 ~ 5J (each service is different, don't study deeply), and it will increase in the future! Two learn together! The advantage is stable income! 40 minutes a day! The first three levels have no money to earn, and it's not easy to mine. After level 4, mines and medicines are easier to mine! Just pick it on a map, and it's time-consuming to change it! Now the brush is very fast
3. When collecting, you can play the next boss, brush Wanling, and take BB by the way. The box must be opened
4. You can learn the skills corresponding to medicine collecting and mining, but it doesn't matter if you don't have much time! Because the proct occupies an area of land, and there is no market for the equipment in the early stage! Now jewelry is popular, but come up with JP to secret silver! So it depends on your own situation. Medicine is mainly for teachers, but it's a waste of time to set up a stall. It depends on everyone's situation. So I say the material is the most stable
method 2: rare animals
1. Rare animal island is full of gold. I walk for an hour or more every day. By the way, I just brush chess every day to earn experience! The length of time depends on personal preference! Those who like to make money should pay more attention. 5 ~ 15 level of original variation BB is better! Generally 1 hour can give 2, 3! The most inferior BB, 5J can always do it? Besides, Wang Ba and dog are very popular in the early stage! I've got a JP bastard and sold 150j
2. BB book! This one has a big head! By the way, any BB on rare animal island has a chance to publish a Book (any book)! Rabbits have also had advanced blood explosions! I generally in 5 ~ 15 level of BB that linger for a long time, in which easy to mutation! But it's more or less about luck! Don't be too serious
3. Alt BB is also useful! And there are too many alts around, it's easy to lead the island protection! By the way, I think the island protection has changed a lot in the past two days! Alt also have growth outstanding! It's all money
4. It's a theorem that there is no relationship between the qualification of the second generation and that of the first generation through the painstaking reproction of BB! Brush chess when the way with BB, and then breeding, there are always good! And the risk is small, the proportion of two garbage is 50%, even if the garbage, if it is silkworm, owl, peacock, also have an opportunity to group! Out of the group, how much is worth it! By the way, where I practice my baby, I usually choose to go to Emei to fight monkeys. The anti side experiment should be the fastest (excluding activities), and there are more chances to bring a trumpet! By the way, good and evil! Switch must see! There may be a sect order! At present, only those who have issued the order can trade the order? Chinese!)
method 3: Kyushu chamber of Commerce
if you do as mentioned above, you can open a shop in Kyushu in a short time, just like it! Put the above materials, books and BBS in, and then how they work depends on your preferences! There are a lot of experiences in this area in the exchange area, which are very good. I can't say anything better than them. Let's have a look for ourselves! In fact, Kyushu is more suitable for people like me who don't have much online time! And the store is open, this is the source of money! Take a look at other people's experience, combined with their own clothes, as long as the use of snacks, who can open a good<
method 4: take part in activities to practice, and make money at the same time
this game has a lot of activities! You can make money while practicing. Of course, I go in line with the spirit of training. Making money is by the way, and it's too lucky to rely on getting rich. So still, don't be too serious! Brush the general gem! A little money is better than nothing! Curfew, gems and skills! Efficient team is very important
method 5: guild task
1. What the guild task must do is not to earn money, but to exchange money, but it is related to the upgrading of life skills, and many guilds are going to the weekend to see your contribution to the business
2. You've made a contribution to the business of the guild. It's not too much to ask for a business position, is it It depends on the operation of your guild and the character of the leader.) I have a lot of business experience! I don't think I need to say more. I usually run at night on weekends! 3 hours 70 ~ 80J (players above level 55) this is not difficult! Some people in the exchange area said that they would sell rice in Suzhou for the second time. This is good. It's easier to get a full ticket! Of course, it depends on where the city you help is! Anyway, I have more experience in this field! Earn less to see other people's post it! Sometimes I'm sleepy and running around 60 J! It's faster to find a friend to lead the team! Xinyou.com
method 6: often visit the stall
buy and sell, earn the difference! This is business! Always meet below the market price of things
in this way, you can open your shop and earn the easy money! Holding 300 ~ 500 gold in hand, at least get rid of poverty, you can buy what you want! Just don't be too serious. People are more popular than dead people! Real JP is not available! Money may not buy it!
monster grade
mineral name / grade
mineral name / grade
mining skill grade
one
unlimited
1-10
copper mine / 1
--
0
Jiange
1-10
copper mine / 1
--
0
Dunhuang
9-16
copper mine / 1
--
0
Jinghu
9-16
copper mine / 1
--
0
Songshan
15-21
copper mine Mineral deposits / 1 < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br /
taihlake Lake Lake
Lake taihlake Lake Lake < br / < 15-21
15-21
copper deposits / 1 < br / < br / < br / < br / < br / < br / < br /
copper deposits / 1 < br / < br / < br /
copper deposits / 2 < br / < br / < br / < br /
Lake Lake taih < br /
Lake Lake taih < br / < br / < br /
Lake taihlake Lake Lake taihlake < br / < br / < br / < 15-21-21 < br / < br / < > Gold / 5 < B The iron ore / 6 < br / < 6 < br / < 5
5 < br / < br / < br /
the north of the wild
45-51 < br /
the iron ore / 6 < br / < br / < 6 < br / < 6 < br / < br / < 6 < br / < br / < 6 < br / < br / < br / < br / < br /
north of the north of the north of the wild
45-51 < br / < 45-51
the iron ore / 6 / 6 < br /
6 < br / < br / < 6 < br /
as you are all < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br / < br/ > I don't know Dao
Tianlong Babu mining
reference: Jinchen online game
In the study of trace element geochemistry, the distribution coefficient is one of the core problems. Without the distribution coefficient data, the quantitative model of trace elements can not be established. The Nernst partition coefficient or simple partition coefficient mentioned above is quoted or discussed in general geochemical literature. It refers to the equilibrium concentration ratio of trace elements between two phases (crystal mineral and liquid melt in most cases) at constant temperature and pressure. According to Nernst's law, the partition coefficient should be composed of two parts: the concentration of trace elements in solid phase (crystalline phase) and liquid phase (matrix) in equilibrium system. In order to measure the concentration of trace elements in these two phases and obtain the partition coefficient, there are two most commonly used methods: direct determination and experimental determination
The direct determination method is also called phenocryst matrix method, which is to determine the distribution coefficient by determining the content of elements in rock phenocryst and matrix. It is not easy to determine the partition coefficients in systems related to magmatism and metamorphism. In fact, little progress has been made before the 1950s. The early determination mainly used the direct determination of natural substances. That is to say, the concentration of elements in two equilibrium coexisting phases of geological body is directly determined, and the distribution coefficient of elements is calculated according to Nernst distribution law. The phenocrysts represent the solid phase in the process of melt crystallization, and the matrix represents the liquid phase, i.e. the magma melt. The ratio of trace element concentration in the two phases is the distribution coefficient of the element. Determination of phenocryst minerals and matrix of volcanic rocks (melt in equilibrium with minerals), or determination of minerals and quenched melt (glass) in lava flow, and determination of coexisting minerals in rocks (mineral / mineral partition coefficient of elements). The method is simple and easy to operate, and provides the approximate concentration range of the distribution coefficient of trace elements. Although the variation range is large, the order of magnitude remains unchanged. The existing problems are as follows: 1) it is difficult to prove whether the whole phenocryst and melt have reached equilibrium, such as the zonal distribution of common crystal growth components in minerals. Although the main components are homogeneous, the concentration of trace elements is zonal, indicating that the equilibrium is incomplete, so the distribution coefficient measured can only be effective or apparent, but not equilibrium; ② It is difficult to obtain pure minerals by manual or magnetic separation, and it is easy to cause matrix pollution for incompatible elements. For transition elements, it will cause trace opaque minerals to be mixed, resulting in wrong distribution coefficient; ③ It is difficult to know under what conditions (temperature and pressure) the system reaches equilibrium and whether the existing phenocrysts have undergone rebalancing or alteration ring magma cooling and upwelling. Since the 1960s, many scholars have devoted themselves to the determination of partition coefficients by experimental methods Experimental determination method through the experiment to make a mineral and a liquid (melt or solution) in equilibrium, or make two minerals reach equilibrium, so that trace elements in the two phases to achieve dissolution equilibrium, and then determine the concentration of elements in the two phases, get the distribution coefficient. It can be divided into two methods: chemical reagent synthesis and direct use of natural materials The second is that it is difficult to separate the mineral from the phase rich in trace elements, and it is also difficult to remove the impurities formed around the crystal ring quenching. The concentration of trace elements used in the experiment will be much higher than that of natural system, which may not be completely suitable for dilute solution system. Wood & Fraser (1978) pointed out that when the element partition coefficient is greater than 1 and obeys Rayleigh fractionation law, the pseudo partition coefficient is greater than the equilibrium partition coefficient. However, if the zonal change of crystal composition is e to the slow diffusion of material in the melt to the growing crystal, the pseudo distribution coefficient will have an abnormally low value. When applying the partition coefficients of trace elements obtained by total analysis of coexisting phases (i.e. single mineral analysis), special attention should be paid to the above conditions. However, they also pointed out that despite the above problems, the pseudo partition coefficient is more accurate than the real equilibrium partition coefficient in reflecting the behavior of elements in the real geological system The main reasons are: 1) the purity of the sample; 2; ② Uniformity of samples; ③ Whether the balance has been reached; ④ Analysis errorthe purity of sample is the first factor of data error, especially for direct determination. For example, the microinclusions in accessory minerals are easy to cause errors in the distribution coefficient. For example, silicotungenite, a by-mineral containing REE, is considered to be the main pollution source of the main mineral, which seriously disturbs the partition coefficient. Cameron & Cameron (1986) reported that epidote, a accessory mineral, greatly affects the REE partition coefficient between amphibole and volcanic glass, including the generation of obvious Eu anomaly. Considering the role of amphibole in the melting process, such a change should be e to the disturbed partition coefficient of amphibole and inclusion, rather than the partition coefficient of pure amphibole (Fig. 5-3)
Fig. 5-3 distribution coefficient of REE between amphibole and volcanic glass
(according to Shaw, 2006)
e to the existence of tiny epidote inclusions in the sample, EU is significantly abnormal, resulting in the distorted distribution coefficient curve of determination
the uniformity of the sample should also be concerned. If the composition of a mineral changes from the core to the edge, the composition of a ground sample cannot quantitatively reflect this change. In addition, this change in composition also indicates a third concern, that is, the chemical equilibrium has not been achieved
In recent decades, the rapid development of analytical methods and technologies, especially the progress of micro beam analysis technology, has greatly improved the quality of partition coefficient measurement, such as modern high-precision micro area measurement technologies such as electron microscope (EMP), ion probe (SIMS) and laser ablation inctively coupled plasma mass spectrometry (LA-ICP-MS), Low or trace element content analysis can be carried out in a mineral or a glass matrix on a polished sheet, and even fluid and melt inclusions with the size of several to tens of microns can be determined to determine the partition coefficient, without the need for physical separation of the sample (zajacz et al., 2008). The experimental measurement of partition coefficient has also been greatly improved. The experimental synthesis technology under high temperature and high pressure has been improved. The application of microbeam technology in this field also has a good prospectfigure 5-4 shows the comparison of the partition coefficients of three trace elements between plagioclase and glass determined earlier and later by Bindeman et al. (1998). Taking RB as an example, the variation range of early data is more than three orders of magnitude, which is useless in the quantitative simulation of trace elements. The new data measured by ion microprobe has a good linear relationship with the content of anorthite in plagioclase
Table 5-1 and table 5-2 are the partition coefficient data of some elements. More detailed data can be found in Irving (1978), rollinson (1993) and Zhao Zhenhua (1997)
Fig. 5-4 diagram of the correlation between the distribution coefficient D of Li, K and Rb between plagioclase and coexisting basalt glass and the content of anorthite in plagioclase. In contrast, the cross is an early determination of volcanic rocks using phenocryst matrix method
Table 5-1 distribution coefficient of elements between minerals and basalt to basalt andesite melt (mark a) and dacite to rhyolite melt (Mark b) at near melting temperature and low pressure (d < sub > I < / sub >
), 2009)
Table 5-2 mineral melt partition coefficients of some elements
(according to Brownlow, 1996)
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