Does Tianlong Babu mine still make money

1. When upgrading a self built skill, you need to upgrade it with gold coins

2. Got diabetes, the first good control of blood sugar, low sugar and high fiber diet, at the same time to quantitative. If possible, it's best to measure the blood sugar value every day. Make sure blood sugar is stable and doesn't change too much.

3. If you want to make money in mining skills, you should at least upgrade to level 6 or above, because only level 6 mines do a little more manual work. You can sell it by hand. Of course, you have to be patient, because you don't have to proce JP. One thing about insurance is that the whole group sells ore, and many people buy it.

4. blockchain technology,
referred to as BT (blockchain
Technology), also known as distributed ledger technology, is an Internet database technology, which is characterized by decentralization, openness and transparency, so that everyone can participate in database records
you can go to oyuan.com to find out

5.

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 error

the 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 prospect

figure 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)

6. Some viruses will slow down the switch and cause the switch to hang up. So even if there is no communication between the two VLANs, the switch will die. The other network will not work properly

but the virus will not run to other VLANs by itself

7. Then you can mine, plant, and make a lot of money a day

8. Tianlong 3 is the most profitable of the royal mausoleum, which can be sold for 200-300 gold (the price is a little different in different districts). If you brush the blood jade with cast patterns, the current price is 900-1000 gold. There are other props to improve the dragon patterns, and the price is also very high. This can be painted every day. At present, Tianlong 3 can be painted four times a day, Fengming Town, juntiancheng Chaojing city and Luofu city
however, if you are not a member of the city's aristocratic family to brush the of the royal mausoleum, the dragon pattern and blood jade you brush are generally bound and can only be used by yourself, not sold. You must be a member of the aristocratic family, and then take part in the battle for the city (3, 6 every week). You can only brush the unbound props after capturing the city.

9. 1. To install the latest security patch for the computer, Microsoft has released patch ms17-010 to fix the system vulnerability of "eternal blue" attack. Please install this security patch as soon as possible at the website of https://technet.microsoft.com/zh-cn/library/security/ms17-010; For Windows XP, 2003 and other machines that Microsoft no longer provides security updates, we can use 360 "NSA Arsenal immune tool" to detect whether there are loopholes in the system, and close the ports affected by the loopholes, so as to avoid being infringed by blackmail software and other viruses. Download address: http://dl.360safe.com/nsa/nsatool.exe
2. Close ports 445, 135, 137, 138 and 139, and close network sharing
3. Strengthen the awareness of network security: don't click the unknown link, don't download the unknown file, don't open the unknown email...
4. Back up the important files in your computer to the mobile hard disk and U disk as soon as possible (regularly in the future), and save the disk offline after the backup
5. It is recommended that users who are still using Windows XP or windows 2003 should upgrade to Windows 7 / windows 10 or windows 2008 / 2012 / 2016 as soon as possible.