Глава 3. СОВМЕСТНОЕ ОДНОВРЕМЕННОЕ ДЕЙСТВИЕ Т‑СРПС и О-СРПС ВОДЫ        154

3.1. Создание механизма диффузионного флюидозамеще­ния в земной коре        154

3.2. Содействие механизма диффузионного флюидозаме­щения заживлению ран и порезов в растениях и живых ор­ганизмах        160

3.3. Регулирование роста растений и живых организмов до определенного размера, определяющего срок их молодости и старости        161

3.4. Избирательная проницаемость мембран в газах и жидкостях        165

Часть II. РОЛЬ СРПС В ГЕОЛОГИЧЕСКИХ ПРОЦЕССАХ        171

Глава 4. ГЕОЛОГИЧЕСКИЙ ПРИМЕР ПРОЦЕССОВ РУДО - И МАГМООБРАЗОВАНИЯ НА ОСНОВЕ ДЕЙСТВИЯ МЕХАНИЗМА ДИФФУЗИОННОГО ФЛЮИДОЗАМЕЩЕНИЯ В ЭКЗО - И ЭНДОКОНТАКТОВОЙ ЗОНЕ ГРАНИТОИДНОГО МАССИВА (карьер Борок г. Новосибирска)        171

4.1. Геологическое строение карьера Борок        171

4.2. Состав пород магматического гранитоидного плутона и их взаимоотношения с вмещающими породами        172

4.3. Состав и текстурно-структурные особенности пород из экзоконтактовой зоны роговиков        179

4.4. Взаимоотношения аплитовых лейкогранитовых жил с сульфидно-кварцевыми и кварц-пироксеновыми прожил­ками в зоне роговиков        190

4.5. Генезис всех видов жил в результате действия еди­ного механизма диффузионного флюидозамещения        193

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Глава 5. ПРОЦЕССЫ МЕТАМОРФИЧЕСКОЙ ПЕРЕКРИСТАЛЛИЗАЦИИ И ПЛАСТИЧЕСКИХ ДЕФОРМАЦИЙ ПОРОД ПРИ ДИНАМОМЕТАМОРФИЗМЕ И СКЛАДЧАТОСТИ        199

Глава 6. ГИДРОГЕОЛОГИЧЕСКИЕ ПРОЦЕССЫ        202

Глава 7. нефтяная геология        205

Глава 8. РЕГУЛИРОВАНИЕ ЗЕМЛЕТРЯСЕНИЙ В ЗЕМНОЙ КОРЕ И СПОСОБ ИХ ПРЕДОТВРАЩЕНИЯ        210

Глава 9. ГЕОКРИОЛОГИЯ        218

Глава 10. ИНЖЕНЕРНАЯ ГЕОЛОГИЯ        220

Глава 11. ОСАДОЧНЫЕ ПРОЦЕССЫ        221

Глава 12. ДИФФЕРЕНЦИАЦИЯ ЗЕМНОЙ КОРЫ И ФОРМИРОВАНИЕ МАТЕРИКОВ В РЕЗУЛЬТАТЕ ДЕЙСТВИЯ МЕХАНИЗМА ДИФФУЗИОННОГО ФЛЮИДОЗАМЕЩЕНИЯ        223

ЗАКЛЮЧЕНИЕ        229

СПИСОК ЛИТЕРАТУРЫ        231

CONTENTS

INTRODUCTION        3

Part 1. FORCE OF DECONDENSATION OF THE SUPERFICIAL LAYER OF WATER – FDSL        8

Chapter 1. TEMPERATURE COMPONENT OF THE FORCE OF DECONDENSATION  OF THE SUPERFICIAL LAYER OF WATER (T-FDSL)        8

1.1. Mistake in modern explanation of the mechanism of forma­tion of surface tension, which did not make possible to discover T-FDSL        8

1.2. Mechanism of origin of T-FDSL by the example of gas        34

1.2.1. Existence of the decondensated superficial layer of gas at the contact with solid walls as a example of action of T-FDSL in gases        34

1.2.2. Explanation of the mechanism of T-FDSL generation  by the example of a gas, in which a partition instantly ap­pears        34

1.2.3. Explanation with using the notion about the probability contour of molecule free run        36

1.2.4. Explanation by the example of baby rattle-box        40

1.2.5. Explanation by the example of peoples chaotic wan­dering in a hall, where they are repulsed from each other and from the walls        41

1.2.6. Explanation by the example of the «blow off» in snow-drift near a wall during snow-storm        42

1.2.7. Explanation of the T-FDSL by the example of a game «in around» or in «two chains»        43

1.2.8. Essence of T-FDSL action in gas        45

1.2.9. Results of T-FDSL action in gases        45

1.3. Mechanism of T-FDSL formation in water        50

1.3.1. Distinction of liquids from gases        50

1.3.2. Peculiarities of termal kinetic motion of molecules in liquids        52

1.3.3. T-FDSL at the boundary of liquid with gas        56

1.3.4. T-FDSL at the boundary of  liquid with solid sub­stances        61

1.4. General physical properties of the superficial layer of water, generated by action of T-FDSL        65

perficial layer has some properties of solid sub­stances        65

1.4.1.1. Formation of surface tension as the force couter­actiong stretching of the superficial layer lengthwise        65

1.4.1.2. Formation of the Deryagin’s disjoining pressure, as the force counteracting rupture of the superficial layer during its compression in transverse direction        66

1.4.1.3. Higher viscosity and strength for shift of the su­perficial layer        72

1.4.1.4. Generation of friction in liquid at the boundary with solid substance        73

1.4.2. Immediate action in natural processes of T-FDSL itself during its generation        75

1.4.3. Manifestation in natural processe of those properties of the superficial layer, which are generated due to action of T-FDSL        79

1.4.4. About experimental investigations of T-FDSL        83

1.5. T-FDSL of solid substances        

Chapter 2. OSMOTIC COMPONENT OF THE FORCE OF DECONDENSATION OF THE SUPERFICIAL LAYER OF WATER – O-FDSL        90

2.1. Existing now view about diffusional or non-dissolving layer of bonded water at the contact with solids        90

2.2. Existing until present time not quite clear the cause of os­mosis        91

2.3. Mistake in molecular-kinetic theory of diffusion, which did not make possible to explain satisfactory the cause of osmosis        97

2.4. New explanation of diffusion as osmotic force, generated as a result of collision of a one sort of dissolved molecules        100

2.4.1. Investigation of the way of chaotic motion of a one molecule in solution of gas        102

2.4.2. Important aspect of diffusion differences in the extent of activity-passivity of diffusing molecules of a gas and of the molecules dissolved in it        107

2.4.3. Explanation of the force effect of osmotic pressure for diffusing gases        108

2.4.4. Experimental verification of diffusion phenomenon as a result of collision of a one sort of molecules of dissolved substances        111

2.4.5. New rule in the molecular-kinetic theory of diffusion        114

2.4.6. New explanation of osmosis and osmotic pressure        116

2.5. Explanation of generation of FDSL osmotic component of water

2.6. Results of action of O-FDSL of water in the nature        119

2.6.1. Generation of microporodiffusional catalytic effect (MDC-effect)        123

2.6.1.1. Essence of the MDC-effect        123

2.6.1.2. Causes of directional movement towards exits from micropores        124

2.6.1.3. Effect O-FDSL in movement of molecules to the exit from mocropores        129

2.6.1.4. Differences in behavior of solvent molecules and dissolved molecules in micropores        131

2.6.1.5. Acceleration of chemical interaction of dissolved molecules with micropore walls, as a result of increase in collision frequency of each individual molecule        132

2.6.1.6. Experimental verification of the MDC-effect        140

2.6.2. Role of the osmotic component of FDSL in the form of MDC-effect in natural phenomena        143

2.6.2.1. Maintaining of constant permeability in the rocks of the Earth”crust during metasomatic processes        143

2.6.2.2. Role of MDC-effect in osmotic phenomena        148

2.6.2.3. Generation of heterogeneous catalysis in the mi­cropores of zeolithes and other microporous mediums        148

2.6.2.4. Initiation of cancer diseases as a result of differ­ent intensity in manifestation of MDC-effect        149

2.6.2.5. Assistance in extraction of mineral substances immediately from rocks by the roots of plants        153

Chapter 3. SIMULTANEOUS AND MUTUAL ACTION OF T-FDSL AND O-FDSL OF WATER        155

3.1. Generation of the mechanism of diffusional fluid replace­ment in the Earth’s crust        155

3.2. Promoting of the diffusional fluid replacement mechanism to healing of wounds and cuts in plants and alive organisms        161

3.3. Regulating of plants and alive organisms growth up to defi­nite size, which controls time of their youth and old age        162

3.4. Selective permeability of membranes in gases and liquids        166

Part 2. ROLE OF FDSL IN GEOLOGICAL PROCESSES        172

Chapter 4.GEOLOGICAL EXAMPLE OF PROCESSES OF ORE-AND MAGMA FORMATION BASING ON ACTION MECHANISM OF DIFFUSION FLUID REPLACEMENT IN THE EXO - AND ENDOCONTACT ZONE OF GRANITOID INTRUSION (quarry Borok, Novosibirsk sity)        172

4.1. Geology of Borok quarry        172

position of rocks of magmatic granitoid pliton and their interrelations with enclosing rocks        174

position and texture-structure peculiarities of the rocks in exocontact zone of hornfels        181

4.4. Interrelations of aplite leucogranite veins with sulphide-quartz veinlets in the hornfels zone        194

4.5. Genesis of all kinds of veins as a result of activity of the single mechanism of diffusional fluid replacement        196

Chapter 5. PROCESSES OF METAMORPHIC RECRYSTALLIZATION AND PLASTIC DEFORMATION DURING DINAMOMETAMORPHISM AND FOLDING        202

Chapter 6. HYDROGEOLOGICAL PROCESSES        205

Chapter 7. OIL GEOLOGY        208

Chapter 8. REGULATING OF EARTHQUAKES IN THE EARTH’S CRUST AND THE METHOD OF THEIR PREVENTION        213

Chapter 9. GEOCRYOLOGY        221        

Chapter 10. ENGINEER GEOLOGY        223

Chapter 11. SEDIMENTARY PROCESSES        224

Chapter 12.  DIFFERENTIATION OF THE EARTH’S CRUST AND FORMATION AS A RESULT OF ACTION OF DIFFUSIONAL FLIUD REPLACEMENT MECHANISM        226

CONCLUSION        232

REFERENCES        234



Научное издание

Леонид Иванович Шабалин

СИЛА РАЗУПЛОТНЕНИЯ ПОВЕРХНОСТНОГО СЛОЯ ВОДЫ И ЕЕ РОЛЬ В ГЕОЛОГИЧЕСКИХ ПРОЦЕССАХ

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