Submit an Article
Become a reviewer
JOURNAL IMPACT FACTOR
2.4
WEB OF SCIENCE (ESCI)
citescore
7.5
scopus

Vol 1 No 4

Previous
Vol 1 No 3
Vol 1 No 4
  • Vol 271
  • Vol 270
  • Vol 269
  • Vol 268
  • Vol 267
  • Vol 266
  • Vol 265
  • Vol 264
  • Vol 263
  • Vol 262
  • Vol 261
  • Vol 260
  • Vol 259
  • Vol 258
  • Vol 257
  • Vol 256
  • Vol 255
  • Vol 254
  • Vol 253
  • Vol 252
  • Vol 251
  • Vol 250
  • Vol 249
  • Vol 248
  • Vol 247
  • Vol 246
  • Vol 245
  • Vol 244
  • Vol 243
  • Vol 242
  • Vol 241
  • Vol 240
  • Vol 239
  • Vol 238
  • Vol 237
  • Vol 236
  • Vol 235
  • Vol 234
  • Vol 233
  • Vol 232
  • Vol 231
  • Vol 230
  • Vol 229
  • Vol 228
  • Vol 227
  • Vol 226
  • Vol 225
  • Vol 224
  • Vol 223
  • Vol 222
  • Vol 221
  • Vol 220
  • Vol 219
  • Vol 218
  • Vol 217
  • Vol 216
  • Vol 215
  • Vol 214
  • Vol 213
  • Vol 212
  • Vol 211
  • Vol 210
  • Vol 209
  • Vol 208
  • Vol 207
  • Vol 206
  • Vol 205
  • Vol 204
  • Vol 203
  • Vol 202
  • Vol 201
  • Vol 200
  • Vol 199
  • Vol 198
  • Vol 197
  • Vol 196
  • Vol 195
  • Vol 194
  • Vol 193
  • Vol 191
  • Vol 190
  • Vol 192
  • Vol 189
  • Vol 188
  • Vol 187
  • Vol 185
  • Vol 186
  • Vol 184
  • Vol 183
  • Vol 182
  • Vol 181
  • Vol 180
  • Vol 179
  • Vol 178
  • Vol 177
  • Vol 176
  • Vol 174
  • Vol 175
  • Vol 173
  • Vol 172
  • Vol 171
  • Vol 170 No 2
  • Vol 170 No 1
  • Vol 169
  • Vol 168
  • Vol 167 No 2
  • Vol 167 No 1
  • Vol 166
  • Vol 165
  • Vol 164
  • Vol 163
  • Vol 162
  • Vol 161
  • Vol 160 No 2
  • Vol 160 No 1
  • Vol 159 No 2
  • Vol 159 No 1
  • Vol 158
  • Vol 157
  • Vol 156
  • Vol 155 No 2
  • Vol 154
  • Vol 153
  • Vol 155 No 1
  • Vol 152
  • Vol 151
  • Vol 150 No 2
  • Vol 150 No 1
  • Vol 149
  • Vol 147
  • Vol 146
  • Vol 148 No 2
  • Vol 148 No 1
  • Vol 145
  • Vol 144
  • Vol 143
  • Vol 140
  • Vol 142
  • Vol 141
  • Vol 139
  • Vol 138
  • Vol 137
  • Vol 136
  • Vol 135
  • Vol 124
  • Vol 130
  • Vol 134
  • Vol 133
  • Vol 132
  • Vol 131
  • Vol 129
  • Vol 128
  • Vol 127
  • Vol 125
  • Vol 126
  • Vol 123
  • Vol 122
  • Vol 121
  • Vol 120
  • Vol 118
  • Vol 119
  • Vol 116
  • Vol 117
  • Vol 115
  • Vol 113
  • Vol 114
  • Vol 112
  • Vol 111
  • Vol 110
  • Vol 107
  • Vol 108
  • Vol 109
  • Vol 105
  • Vol 106
  • Vol 103
  • Vol 104
  • Vol 102
  • Vol 99
  • Vol 101
  • Vol 100
  • Vol 98
  • Vol 97
  • Vol 95
  • Vol 93
  • Vol 94
  • Vol 91
  • Vol 92
  • Vol 85
  • Vol 89
  • Vol 87
  • Vol 86
  • Vol 88
  • Vol 90
  • Vol 83
  • Vol 82
  • Vol 80
  • Vol 84
  • Vol 81
  • Vol 79
  • Vol 78
  • Vol 77
  • Vol 76
  • Vol 75
  • Vol 73 No 2
  • Vol 74 No 2
  • Vol 72 No 2
  • Vol 71 No 2
  • Vol 70 No 2
  • Vol 69 No 2
  • Vol 70 No 1
  • Vol 56 No 3
  • Vol 55 No 3
  • Vol 68 No 2
  • Vol 69 No 1
  • Vol 68 No 1
  • Vol 67 No 1
  • Vol 52 No 3
  • Vol 67 No 2
  • Vol 66 No 2
  • Vol 64 No 2
  • Vol 64 No 1
  • Vol 54 No 3
  • Vol 65 No 2
  • Vol 66 No 1
  • Vol 65 No 1
  • Vol 53 No 3
  • Vol 63 No 1
  • Vol 61 No 1
  • Vol 62 No 1
  • Vol 63 No 2
  • Vol 62 No 2
  • Vol 61 No 2
  • Vol 59 No 2
  • Vol 60 No 2
  • Vol 51 No 3
  • Vol 60 No 1
  • Vol 49 No 3
  • Vol 50 No 3
  • Vol 59 No 1
  • Vol 57 No 2
  • Vol 58 No 2
  • Vol 58 No 1
  • Vol 56 No 2
  • Vol 57 No 1
  • Vol 55 No 2
  • Vol 48 No 3
  • Vol 56 No 1
  • Vol 47 No 3
  • Vol 55 No 1
  • Vol 54 No 2
  • Vol 53 No 2
  • Vol 54 No 1
  • Vol 52 No 2
  • Vol 46 No 3
  • Vol 53 No 1
  • Vol 52 No 1
  • Vol 51 No 2
  • Vol 51 No 1
  • Vol 50 No 2
  • Vol 49 No 2
  • Vol 48 No 2
  • Vol 50 No 1
  • Vol 49 No 1
  • Vol 45 No 3
  • Vol 47 No 2
  • Vol 44 No 3
  • Vol 43 No 3
  • Vol 42 No 3
  • Vol 48 No 1
  • Vol 46 No 2
  • Vol 45 No 2
  • Vol 46 No 1
  • Vol 47 No 1
  • Vol 44 No 2
  • Vol 43 No 2
  • Vol 41 No 3
  • Vol 42 No 2
  • Vol 39 No 3
  • Vol 37 No 3
  • Vol 45 No 1
  • Vol 41 No 2
  • Vol 39 No 2
  • Vol 44 No 1
  • Vol 38 No 2
  • Vol 37 No 2
  • Vol 38 No 3
  • Vol 43 No 1
  • Vol 42 No 1
  • Vol 41 No 1
  • Vol 40
  • Vol 39 No 1
  • Vol 36 No 2
  • Vol 35 No 2
  • Vol 38 No 1
  • Vol 35 No 3
  • Vol 34 No 2
  • Vol 34 No 3
  • Vol 33 No 2
  • Vol 36 No 1
  • Vol 37 No 1
  • Vol 36 No 3
  • Vol 35 No 1
  • Vol 34 No 1
  • Vol 32 No 3
  • Vol 33 No 3
  • Vol 32 No 2
  • Vol 33 No 1
  • Vol 31
  • Vol 30 No 3
  • Vol 30 No 2
  • Vol 30 No 1
  • Vol 32 No 1
  • Vol 29 No 3
  • Vol 29 No 1
  • Vol 29 No 2
  • Vol 28
  • Vol 27 No 1
  • Vol 27 No 2
  • Vol 26 No 2
  • Vol 26 No 1
  • Vol 25 No 2
  • Vol 25 No 1
  • Vol 23
  • Vol 24
  • Vol 15 No 16
  • Vol 22
  • Vol 20
  • Vol 17 No 18
  • Vol 21
  • Vol 19
  • Vol 13 No 3
  • Vol 14
  • Vol 13 No 2
  • Vol 12 No 3
  • Vol 12 No 2
  • Vol 13 No 1
  • Vol 12 No 1
  • Vol 11 No 3
  • Vol 11 No 2
  • Vol 10 No 3
  • Vol 10 No 2
  • Vol 11 No 1
  • Vol 9 No 2
  • Vol 10 No 1
  • Vol 9 No 1
  • Vol 8
  • Vol 7 No 3
  • Vol 7 No 2
  • Vol 7 No 1
  • Vol 6 No 2
  • Vol 6 No 1
  • Vol 5 No 4-5
  • Vol 5 No 2-3
  • Vol 5 No 1
  • Vol 4 No 5
  • Vol 4 No 4
  • Vol 4 No 3
  • Vol 4 No 2
  • Vol 3
  • Vol 4 No 1
  • Vol 2 No 5
  • Vol 2 No 4
  • Vol 2 No 3
  • Vol 2 No 1
  • Vol 2 No 2
  • Vol 1 No 5
  • Vol 1 No 4
  • Vol 1 No 3
  • Vol 1 No 2
  • Vol 1 No 1
Geology
  • Date submitted
    1908-06-03
  • Date accepted
    1908-08-13
  • Date published
    1908-12-01

Hypoparallel aragonite intergrowth from Bilin

Article preview

Among the deviations from the laws characteristic of real (ideal), that is, completely crystalline-homogeneous individuals, small deviations are often noticed both in the position of the edges and in general in the intergrowth of subindividuals.

How to cite: Fedorov Y.S. Hypoparallel aragonite intergrowth from Bilin // Journal of Mining Institute. 1908. Vol. № 4 1. p. 317-318.
Without section
  • Date submitted
    1908-06-25
  • Date accepted
    1908-08-22
  • Date published
    1908-12-01

About the influence of the concentration of reacting solutions on the appearance and structure of sediments

Article preview

This work, although it represents only one of the most important links in my extensive work on the states of matter, which I publish, for certain reasons, in German, is a completely accomplished independent whole. This work treats the question of the influence of the concentration of reacting solutions on the appearance and structure of sediments - a question that has not yet been completely developed in science, except for a few fragmentary observations.

How to cite: von-Weymarn P.P. About the influence of the concentration of reacting solutions on the appearance and structure of sediments // Journal of Mining Institute. 1908. Vol. № 4 1. p. 239-262.
Without section
  • Date submitted
    1908-06-20
  • Date accepted
    1908-08-02
  • Date published
    1908-12-01

Electrical conductivity of magnesium-lead alloys

Article preview

The study of the electrical conductivity of metal alloys makes it possible, along with other physical research methods, to judge about their chemical nature. Matthiessen, who carried out classical research in this area, was the first to try to find the relationship between the composition and electrical conductivity of alloys. But at that time (60s and 70s of the last century) ideas about the nature of alloys and information about their structure were so imperfect that it is not always possible to agree with the author’s conclusions on this issue.

How to cite: Stepanov N.I. Electrical conductivity of magnesium-lead alloys // Journal of Mining Institute. 1908. Vol. № 4 1. p. 263-274.
Without section
  • Date submitted
    1908-06-17
  • Date accepted
    1908-08-02
  • Date published
    1908-12-01

New proof of the fundamental theorem of Algebra

Article preview

We will change x along a closed curve in the positive direction. A full description of the proof is in the article.

How to cite: Dolbny I.P. New proof of the fundamental theorem of Algebra // Journal of Mining Institute. 1908. Vol. № 4 1. p. 275-276.
Without section
  • Date submitted
    1908-06-24
  • Date accepted
    1908-08-15
  • Date published
    1908-12-01

On a class of reducible hyperelliptic integrals

Article preview

Let us take the integral and find a substitution of the lowest degree, through which we achieve the reduction of this integral to an elliptic one.

How to cite: Dolbny I.P. On a class of reducible hyperelliptic integrals // Journal of Mining Institute. 1908. Vol. № 4 1. p. 277-278.
Without section
  • Date submitted
    1908-06-28
  • Date accepted
    1908-08-12
  • Date published
    1908-12-01

Illustration of crystal structure with vector circles

Article preview

In the article “Precise imagery of space points on a plane”, the problem of such an image in three different elements is solved: vectorial and ordinary circles, and in parallel vectors. The practical application of images in parallel vectors of a system of mines is also given there. I will now show an essential application of the theory to the representation by vectorial circles of the spatial lattices of each structurally studied crystal.

How to cite: Fedorov Y.S. Illustration of crystal structure with vector circles // Journal of Mining Institute. 1908. Vol. № 4 1. p. 279-294.
Without section
  • Date submitted
    1908-06-07
  • Date accepted
    1908-08-15
  • Date published
    1908-12-01

Some of the rock samples from graphite deposits belonging to the mineralogical collection of the Mining Museum

Article preview

The studied samples are graphite-hosting rocks from various graphite deposits: the Mariinsky mine at the Botogolsky Golets (Aliberovskoye deposit), the Barrowdelsky mine in Cumberland and two Ural deposits - one near the Sysertsky plant; the location of the other deposit is unknown - probably from the Ilmen Mountains.

How to cite: Zavaritsky A.N. Some of the rock samples from graphite deposits belonging to the mineralogical collection of the Mining Museum // Journal of Mining Institute. 1908. Vol. № 4 1. p. 295-301.
Without section
  • Date submitted
    1908-06-11
  • Date accepted
    1908-08-09
  • Date published
    1908-12-01

Construction of a curved surface of the 2nd order (conoseconds) from imaginary pairs of points or an imaginary conic section.

Article preview

We know that from two given points e with e' and a conical section K on the plane, we can reproduce a curved surface of the 2nd order, if from these points we take one e as the center of the second of the rays, and the second e' as the center of the second of the planes and bring these two seconds into a correlative relation so that the ray ea (a point on the conic section plane) will be considered correlative to the plane e'A, where A is the polar of the point a with respect to the conic section K. It is known that in such a surface a set of rays and their correlative planes.

How to cite: Fedorov Y.S. Construction of a curved surface of the 2nd order (conoseconds) from imaginary pairs of points or an imaginary conic section. // Journal of Mining Institute. 1908. Vol. № 4 1. p. 302-304.
Without section
  • Date submitted
    1908-06-04
  • Date accepted
    1908-08-29
  • Date published
    1908-12-01

Construction of curved surfaces of the second order (conoseconds) and a full hexahedron.

Article preview

No matter how elegant the construction of conic sections using Pascal's theorem is, it does not have sufficient generality, since it is applicable only for five real points of a curve, and in practical application it is more difficult than some other methods.

How to cite: Fedorov Y.S. Construction of curved surfaces of the second order (conoseconds) and a full hexahedron. // Journal of Mining Institute. 1908. Vol. № 4 1. p. 305-312.
Without section
  • Date submitted
    1908-06-17
  • Date accepted
    1908-08-27
  • Date published
    1908-12-01

On the preparation of salts of alkali and alkaline earth metals in so-called colloidal amorphous formations that are highly crystallizing and highly soluble in water

Article preview

In my numerous reports and articles published in Russian and German from 1905 to 1908, I experimentally proved that the type and structure of sediment of any body can be changed at the will of the researcher.

How to cite: von-Weymarn P.P. On the preparation of salts of alkali and alkaline earth metals in so-called colloidal amorphous formations that are highly crystallizing and highly soluble in water // Journal of Mining Institute. 1908. Vol. № 4 1. p. 313-314.
Without section
  • Date submitted
    1908-06-10
  • Date accepted
    1908-08-19
  • Date published
    1908-12-01

Crystalline-liquid state as a general property of matter

Article preview

In my previous studies, published in 1905-1908 in Russian and German, I showed that any body, both simple and complex chemical composition, can be obtained: in good clear crystals; in an “irreversible” colloidal state (in the form of sols and “irreversible” colloidal-amorphous sediments); in a “reversible” colloidal state (by rapid cooling and increasing association of dissolved particles into the solution).

How to cite: von-Weymarn P.P. Crystalline-liquid state as a general property of matter // Journal of Mining Institute. 1908. Vol. № 4 1. p. 314-315.
Without section
  • Date submitted
    1908-06-01
  • Date accepted
    1908-08-14
  • Date published
    1908-12-01

A note about one property of stereographic projection

Article preview

I consider it useful to note one property of stereographic projection, which it does not open up new ways for solving problems, still can contribute to greater accuracy in solving some of them.

How to cite: Fedorov Y.S. A note about one property of stereographic projection // Journal of Mining Institute. 1908. Vol. № 4 1. p. 316.
Without section
  • Date submitted
    1908-06-10
  • Date accepted
    1908-08-20
  • Date published
    1908-12-01

On the issue of the formation of telluric iron from bog ores

Article preview

n 1891, 20 versts northeast of Vologda, near the Church of St. Nicholas of Vozimsky (near Lake Kubinskoe), a piece of iron was found under a peat mass in the thickness of bog ore, shallow from the surface. It was originally coated with a loose coating of ocher and immersed in bog ore; its weight together with ocher was 1100 grams. In some places it was permeated with rust to a certain depth. Freed from the ocher shell, it had the shape of a spherical sector measuring about 10 centimeters wide and about 5 centimeters thick; it was veined and in places contained fine granular inclusions of ocher magnetic ironstone.

How to cite: Kupffer A.E. On the issue of the formation of telluric iron from bog ores // Journal of Mining Institute. 1908. Vol. № 4 1. p. 318.