Ch 2: The S/C Environment and its Effect on Design 1/2 Flashcards

1
Q

Main sources of noise and vibration during launch

A
  • LV engines

- aerodynamic buffeting in lower atmosphere

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2
Q

aerodynamic buffeting

A

Buffeting is a high-frequency instability, caused by airflow separation or shock wave oscillations from one object striking another. It is caused by a sudden impulse of load increasing. It is a random forced vibration.

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3
Q

Peak vibration/acoustic levels during launch

A
  1. LIFT-OFF: rocket motor + ground reflection of exhaust products -> primary vibration to PL through structural elements and secondary through the launch shroud
  2. TRANSONIC FLIGHT
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4
Q

peak acceleration depending on LV

A

HIGH PEAK ACC - low-mass LVs (obvs), air-launched

multistage - peak at seperation

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5
Q

what is the thermal environment during launch determined by?

A

launch shroud temperature

after ejection - friction, but by then low atmospheric density

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6
Q

determining the temperature reached during launch

A

specific heat of the shroud material

friction heating vs radiative + convective heat loss

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7
Q

depressurisation rate

A

venting ports in shrouds

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8
Q

venting ports esp. required where in PL?

A

electronic boxes

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9
Q

EMI

A

EM interference; huge hazard during launch

-> PL prop ignition etc

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10
Q

Sun mass

A

~2e30 kg

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11
Q

Sun radiated light peak λ

A

~460 nm

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12
Q

Interstellar gas density

A

~3 atoms/cm^3

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13
Q

Sun surface temperature

A

~5800 K

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14
Q

Sun radiation - regions causing dips from the BB curve

A

CHROMOSPHERE: lower atmosphere, few thousand kms above the photosphere, increasing temperature to ~10e3 K -> enhanced UV emission

CORONA: upper atmosphere, extends to a few solar radii, 2e6 K -> X-rays emission

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15
Q

solar wind - what, where from, physical properties @ Earth

A

flow of plasma expelled at high velocity; outermost layer of solar atmosphere

@ Earth: ~450 km/s, ~9 protons/cm^3, kinetic temp ~100e3 K

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16
Q

sunspots

A

regions of the solar disk cooler than the rest

large number of sunspots -> enhanced solar activity primarily @ radio, X and γ - solar flares usually occur near sunspots

17
Q

Zürich sunspot number Rz

A

quantifies overall number of sunspots at given time

Rz = K (10g + f)

K - normalisation factor depending on observing instrument
g - number of sunspot groups present
f - number of sunspots exhibiting umbrae

18
Q

sunspot regions

A

umbra - middle, darkest
penumbra - around, lighter
pores - small dark spots around

19
Q

components of solar flux @ Earth

A
  1. ~20 minutes after the flare: first heightened EM emissions
  2. ~1 day after the flare: enhanced solar wind components, ~1e3 km/s
20
Q

lower atmosphere - approx boundary, difference to higher

A

~86 km

sufficiently turbulent to be homogeneous (bc gas mixture)

above that, the homogeneity is disturbed by photochemical processes

21
Q

upper atmosphere processes

A

the homogeneity of atmosphere starts being disturbed by photochemical processes from ~86 km

  • > solar UV radiation causes dissociation of oxygen
  • > by ~120 km all atmospheric species decoupled from others

//txtbook - eq of the diffusive equilibrium (number density, molecular weight, altitude, vertical transport velocity, molecular and thermal diffusion coeff, atmospheric temperature, R, g);

can be simplified assuming no vertical transport and negligible thermal diffusion -> hydrostatic equilibrium; number density profile(atmospheric temp)

22
Q

exospheric temperature T_inf

A

increase in solar activity -> rise in T_inf

also geomagnetism

23
Q

how does solar activity cause lower lifespan for SC in LEO?

A

solar activity -> lower atmospheric density (~T^-1)

//txtbook - models to estimate orbit decay

24
Q

ratio of atmosphere/interplanetary medium at GEO

A

~1

25
Q

SC - atomic/molecular collisions

A

v rare above 200 km (mean free path 240 m and rises fast)

  • > heat exchange virtually only through radiation - primary: solar radiation ~1371 W/m^2, secondary: Earth albedo, Earthshine ~200 W/m^2
  • > aerodynamics based on free molecular flow (Ch. 4)
26
Q

ionosphere

A

> 86 km

increased plasma density caused by photoionisation by incident UV photons

27
Q

plasma influence on wave propagation

A

waves with frequency lower than plasma frequency fp~9000*sqrt(ne) cannot propagate (units???)

Faraday rotation - polarisation of EM wave passing through plasma due to an EM field when EMF present

28
Q

sources of Earth MF

A
  1. core currents -> dominant MF at surface
  2. differential motion of electrons and ions in the magnetosphere -> MF at higher altitudes

also solar wind

29
Q

Earth MF constant or?

A
  • decreases by ~0.05% pa

- weakest @ the equator

30
Q

Van Allen belts structure

A

primary: protons and electrons following Earth MF lines
secondary: fluxes of heavy ions (He, N, O) - atmospheric density dependant on solar and geomagnetic activity

31
Q

what are heavy ions?

A

in nuclearphysics, any particle with one or more units ofelectric charge and a mass exceeding that of thehelium-4 nucleus(alpha particle).

32
Q

South Atlantic Anomaly

A

region of enhanced radiation in which parts of the radiation belt are brought to lower altitudes

cause: geomagnetic =/= rotation axis (offset, tilt)

33
Q

radiation belt - dangers to SC

A
  • > collision with semiconductor lattice causes displacement causes local ionisation and energy structure disruption -> arrays energy conversion efficiency
  • > ionisation -> impulsive charge release -> SEU (single-upset event)
34
Q

influence of electrons and protons depending on orbit

A

<800 km - mostly protons
>800 km - mostly electrons

protons - much higher mass -> more effective