Calculation
My Calculation
Slovensko
Structure input data
MASS [m]:
t
STIFFNESS [k]:
kN/m
CRITICAL DAMPING RATIO [ξ]:
NATURAL PERIOD [T]:
s
NATURAL FREQUENCY [ω]:
s
-1
DAMPING COEFFICIENT [c]:
kNs/m
Load input data
DYNAMIC LOAD PROBLEM TYPE:
HARMONIC LOAD
IMPACT LOAD
CONSTANT LOAD
EARTHQUAKE LOAD
CONSTANT LOAD WITH AN IMPACT OF LOADING TIME
NATURAL OSCILLATION
MAXIMUM LOAD [f]:
kN
OBSERVATION TIME [t]:
s
TIME TO CONSTANT LOAD [t
r
]:
s
STIMULATION FREQUENCY [Ω]:
s
-1
IMPACT LOAD TYPE:
RECTANGULAR
TRIANGULAR
t_start:
s
t_f_max:
s
t_end:
s
EARTHQUAKE:
Helena, Montana-01 (Mw = 6 , Strike-Slip, vs30 = 659.6 m/s, d_epi = 6.31 km, d_hypo = 8.71 km)
Helena, Montana-02 (U = 6 , vs30 = 659.6 m/s, d_epi = 6.31 km, d_hypo = km)
Santa Barbara (Mw = 5.92 , Reverse-Oblique, vs30 = 514.99 m/s, d_epi = 3.2 km, d_hypo = 13.1 km)
Norcia, Italy (Mw = 5.9 , Normal, vs30 = 659.6 m/s, d_epi = 4.29 km, d_hypo = 7.37 km)
Mammoth Lakes-01 (Mw = 6.06 , Normal-Oblique, vs30 = 338.54 m/s, d_epi = 1.43 km, d_hypo = 9.11 km)
Mammoth Lakes-03 (Mw = 5.91 , Strike-Slip, vs30 = 338.54 m/s, d_epi = 5.9 km, d_hypo = 17.05 km)
Westmorland (Mw = 5.9 , Strike-Slip, vs30 = 191.14 m/s, d_epi = 8.62 km, d_hypo = 8.92 km)
Westmorland (Mw = 5.9 , Strike-Slip, vs30 = 193.67 m/s, d_epi = 7.02 km, d_hypo = 7.38 km)
N. Palm Springs (Mw = 6.06 , Reverse-Oblique, vs30 = 345.42 m/s, d_epi = 6.28 km, d_hypo = 12.66 km)
N. Palm Springs (Mw = 6.06 , Reverse-Oblique, vs30 = 345.42 m/s, d_epi = 4.24 km, d_hypo = 11.79 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 550 m/s, d_epi = 6.77 km, d_hypo = 16.09 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 367.53 m/s, d_epi = 9.89 km, d_hypo = 17.64 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 308.65 m/s, d_epi = 7.5 km, d_hypo = 16.42 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 468.18 m/s, d_epi = 2.86 km, d_hypo = 14.88 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 349.43 m/s, d_epi = 9.05 km, d_hypo = 17.18 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 401.37 m/s, d_epi = 4.77 km, d_hypo = 15.36 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 379.43 m/s, d_epi = 8.59 km, d_hypo = 16.94 km)
Whittier Narrows-01 (Mw = 5.99 , Reverse-Oblique, vs30 = 298.68 m/s, d_epi = 4.16 km, d_hypo = 15.18 km)
Northridge-02 (Mw = 6.05 , vs30 = 297.71 m/s, d_epi = 6.55 km, d_hypo = 8.88 km)
Chi-Chi, Taiwan-02 (Mw = 5.9 , Reverse, vs30 = 549.43 m/s, d_epi = 5.49 km, d_hypo = 9.7 km)
Denizli (Mw = 6.1 , Normal, vs30 = 345.94 m/s, d_epi = 10 km, d_hypo = 11 km)
Lazio Abruzzo (Mw = 5.9 , Normal, vs30 = 659.6 m/s, d_epi = 5 km, d_hypo = 12 km)
Kalamata (Mw = 6 , Normal, vs30 = 401.44 m/s, d_epi = 10 km, d_hypo = 10 km)
Umbria Marche (Mw = 6 , Normal, vs30 = 142.64 m/s, d_epi = 5 km, d_hypo = 8 km)
Duzce 2 (Aftershock) (Mw = 6 , Normal, vs30 = 347.9 m/s, d_epi = 9 km, d_hypo = 14 km)
Ardal (Mw = 6 , Reverse, vs30 = 757 m/s, d_epi = 7 km, d_hypo = 11 km)
Firuzabad (Mw = 5.9 , Strike-Slip, vs30 = 696 m/s, d_epi = 6 km, d_hypo = 11 km)
DIRECTION:
H1
H2
V
start displacement:
m
initial velocity:
m/s
Analysis input data
ANALYSIS METHOD:
NEWMARK METHOD
CENTRAL DIFFERENCE METHOD
DUHAMEL INTEGRAL
WILSON-ϑ METHOD
TIME STEP [∆t]:
s
NEWMARK PARAMETERS:
γ =
β =
WILSON-ϑ PARAMETER:
ϑ =
CALCULATE