The delicate balance in the universe - What if this balance is violated?
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| The delicate balance in the universe |
| What if this balance is violated? |
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The following table shows what would happen if the delicate balance in each individual detail of this vast universe is violated. This obligates us to thank our God who bestows upon us with this delicate balance so that we can live in this universe.
Allah says in Quran "Lo! We have created every thing by measure" (Quran 54:49)
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From a paper “Limits for the Universe” by Hugh Ross, Ph.D |
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1 |
Gravitational coupling constant |
If larger: |
No stars less than 1.4 solar masses, hence short stellar life spans |
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If smaller: |
No stars more than 0.8 solar masses, hence no heavy element production |
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2 |
Strong nuclear force coupling constant |
If larger: |
No hydrogen; nuclei essential for life are unstable |
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If smaller: |
No elements other than hydrogen |
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3 |
Weak nuclear force coupling constant |
If larger: |
All hydrogen is converted to helium in the big bang, hence too much heavy elements |
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If smaller: |
No helium produced from big bang, hence not enough heavy elements |
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4 |
Electromagnetic coupling constant |
If larger: |
No chemical bonding; elements more massive than boron are unstable to fission |
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If smaller: |
No chemical bonding |
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5 |
Ratio of protons to electrons formation |
If larger: |
Electromagnetism dominates gravity preventing galaxy, star, and planet formation |
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If smaller: |
Electromagnetism dominates gravity preventing galaxy, star, and planet formation |
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6 |
Ratio of electron to proton mass |
If larger: |
No chemical bonding |
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If smaller: |
No chemical bonding |
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7 |
Expansion rate of the universe |
If larger: |
No galaxy formation |
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If smaller: |
Universe collapses prior to star formation |
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8 |
Entropy level of universe |
If larger: |
No star condensation within the proto-galaxies |
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If smaller: |
No proto-galaxy formation |
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9 |
Mass density of the universe |
If larger: |
Too much deuterium from big bang, hence stars burn too rapidly |
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If smaller: |
No helium from big bang, hence not enough heavy elements |
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10 |
Age of the universe |
If older: |
No solar-type stars in a stable burning phase in the right part of the galaxy |
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If younger: |
Solar-type stars in a stable burning phase would not yet have formed |
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11 |
Initial uniformity of radiation |
If smoother: |
Stars, star clusters, and galaxies would not have formed |
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If coarser: |
Universe by now would be mostly black holes and empty space |
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12 |
Average distance between stars |
If larger: |
Heavy element density too thin for rocky planet production |
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If smaller: |
Planetary orbits become destabilized |
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13 |
Solar luminosity |
If increases too soon: |
Runaway green house effect |
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If increases too late: |
Frozen oceans |
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14 |
Fine structure constant* |
If larger: |
No stars more than 0.7 solar masses |
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If smaller: |
No stars less then 1.8 solar masses |
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15 |
Decay rate of the proton |
If greater: |
Life would be exterminated by the release of radiation |
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If smaller: |
Insufficient matter in the universe for life |
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16 |
12C to 16O energy level ratio |
If larger: |
Insufficient oxygen |
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If smaller: |
Insufficient carbon |
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17 |
Decay rate of 8Be |
If slower: |
Heavy element fusion would generate catastrophic explosions in all the stars |
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If faster: |
No element production beyond beryllium and, hence, no life chemistry possible |
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18 |
Mass difference between the neutron and the proton |
If greater: |
Protons would decay before stable nuclei could form |
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If smaller: |
Protons would decay before stable nuclei could form |
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19 |
Initial excess of nucleons over anti-nucleons |
If greater: |
Too much radiation for planets to form |
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If smaller: |
Not enough matter for galaxies or stars to form |
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20 |
Galaxy type |
If too elliptical: |
Star formation ceases before sufficient heavy element buildup for life chemistry |
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If too irregular: |
Radiation exposure on occasion is too severe and/or heavy elements for life chemistry are not available |
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21 |
Parent star distance from center of galaxy |
If farther: |
Quantity of heavy elements would be insufficient to make rocky planets |
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If closer: |
Stellar density and radiation would be too great |
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22 |
Number of stars in the planetary system |
If more than one: |
Tidal interactions would disrupt planetary orbits |
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If less than one: |
Heat produced would be insufficient for life |
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23 |
Parent star birth date |
If more recent: |
Star would not yet have reached stable burning phase |
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If less recent: |
Stellar system would not yet contain enough heavy elements |
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24 |
Parent star mass |
If greater: |
Luminosity would change too fast; star would burn too rapidly |
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If less: |
Range of distances appropriate for life would be too narrow; tidal forces would disrupt the rotational period for a planet of the right distance; uv radiation would be inadequate for plants to make sugars and oxygen |
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25 |
Parent star age |
If older: |
Luminosity of star would change too quickly |
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If younger: |
Luminosity of star would change too quickly |
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26 |
Parent star color |
If redder: |
Photosynthetic response would be insufficient |
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If bluer: |
Photosynthetic response would be insufficient |
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27 |
Supernovae eruptions |
If too close: |
Life on the planet would be exterminated |
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If too far: |
Not enough heavy element ashes for the formation of rocky planets |
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If too infrequent: |
Not enough heavy element ashes for the formation of rocky planets |
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If too frequent: |
Life on the planet would be exterminated |
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28 |
White dwarf binaries |
If too few: |
Insufficient fluorine produced for life chemistry to proceed |
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If too many: |
Disruption of planetary orbits from stellar density; life on the planet would be exterminated |
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29 |
Surface gravity (escape velocity) |
If stronger: |
Atmosphere would retain too much ammonia and methane |
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If weaker: |
Planet's atmosphere would lose too much water |
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30 |
Distance from parent star |
If farther: |
Planet would be too cool for a stable water cycle |
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If closer: |
Planet would be too warm for a stable water cycle |
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31 |
Inclination of orbit |
If too great: |
Temperature differences on the planet would be too extreme |
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32 |
Orbital eccentricity |
If too great: |
Seasonal temperature differences would be too extreme |
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33 |
Axial tilt |
If greater: |
Surface temperature differences would be too great |
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If less: |
Surface temperature differences would be too great |
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34 |
Rotation period |
If longer: |
Diurnal temperature differences would be too great |
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If shorter: |
Atmospheric wind velocities would be too great |
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35 |
Gravitational interaction with a moon |
If greater: |
Tidal effects on the oceans, atmosphere, and rotational period would be too severe |
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If less: |
Orbital obliquity changes would cause climatic instabilities |
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36 |
Magnetic field |
If stronger: |
Electromagnetic storms would be too severe |
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If weaker: |
Inadequate protection from hard stellar radiation |
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37 |
Thickness of crust |
If thicker: |
Too much oxygen would be transferred from the atmosphere to the crust |
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If thinner: |
Volcanic and tectonic activity would be too great |
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38 |
Albedo (ratio of reflected light to total amount falling on surface) |
If greater: |
Runaway ice age would develop |
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If less: |
Runaway green house effect would develop |
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39 |
Oxygen to nitrogen ratio in atmosphere |
If larger: |
Advanced life functions would proceed too quickly |
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If smaller: |
Advanced life functions would proceed too slowly |
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40 |
Carbon dioxide level in atmosphere |
If greater: |
Runaway greenhouse effect would develop |
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If less: |
Plants would not be able to maintain efficient photosynthesis |
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41 |
Water vapor level in atmosphere |
If greater: |
Runaway greenhouse effect would develop |
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If less: |
Rainfall would be too meager for advanced life on the land |
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42 |
Ozone level in atmosphere |
If greater: |
Surface temperatures would be too low |
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If less |
Surface temperatures would be too high; there would be too much uv radiation at the surface |
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43 |
Atmospheric electric discharge rate |
If greater: |
Too much fire destruction would occur |
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If less: |
Too little nitrogen would be fixed in the atmosphere |
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44 |
Oxygen quantity in atmosphere |
If greater: |
Plants and hydrocarbons would burn up too easily |
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If less: |
Advanced animals would have too little to breathe |
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45 |
Oceans to continents ratio |
If greater: |
Diversity and complexity of life-forms would be limited |
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If smaller: |
diversity and complexity of life-forms would be limited |
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46 |
Soil materializations |
If too nutrient poor: |
diversity and complexity of life-forms would be limited |
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If too nutrient rich: |
Diversity and complexity of life-forms would be limited |
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47 |
Seismic activity |
If greater: |
Too many life-forms would be destroyed |
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If less: |
Nutrients on ocean floors (from river runoff) would not be recycled to the continents through tectonic uplift |
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From a paper “Limits for the Universe” by Hugh Ross, Ph.D |
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