cpdef dsmincurb( float len12,
float azm1,
float dip1,
float azm2,
float dip2):
"""
dsmincurb(len12, azm1, dip1, azm2, dip2)
Desurvey one interval with minimum curvature
Given a line with length ``len12`` and endpoints p1,p2 with
direction angles ``azm1, dip1, azm2, dip2``, this function returns
the differences in coordinate ``dz,dn,de`` of p2, assuming
p1 with coordinates (0,0,0)
Parameters
len12, azm1, dip1, azm2, dip2: float
len12 is the length between a point 1 and a point 2.
azm1, dip1, azm2, dip2 are direction angles azimuth, with 0 or
360 pointing north and dip angles measured from horizontal
surface positive downward. All these angles are in degrees.
Returns
-
out : tuple of floats, ``(dz,dn,de)``
Differences in elevation, north coordinate (or y) and
east coordinate (or x) in an Euclidean coordinate system.
See Also
ang2cart,
Notes
-
The equations were derived from the paper:
http://www.cgg.com/data//1/rec_docs/2269_MinimumCurvatureWellPaths.pdf
The minimum curvature is a weighted mean based on the
dog-leg (dl) value and a Ratio Factor (rf = 2*tan(dl/2)/dl )
if dl is zero we assign rf = 1, which is equivalent to balanced
tangential desurvey method. The dog-leg is zero if the direction
angles at the endpoints of the desurvey intervals are equal.
Example
>>> dsmincurb(len12=10, azm1=45, dip1=75, azm2=90, dip2=20)
(7.207193374633789, 1.0084573030471802, 6.186459064483643)
"""
# output
cdef:
float dz
float dn
float de
# internal
cdef:
float i1
float a1
float i2
float a2
float DEG2RAD
float rf
float dl
DEG2RAD=3.141592654/180.0
i1 = (90 - dip1) * DEG2RAD
a1 = azm1 * DEG2RAD
i2 = (90 - dip2) * DEG2RAD
a2 = azm2 * DEG2RAD
# calculate the dog-leg (dl) and the Ratio Factor (rf)
dl = acos(cos(i2-i1)-sin(i1)*sin(i2)*(1-cos(a2-a1)))
if dl!=0.:
rf = 2*tan(dl/2)/dl # minimum curvature
else:
rf=1 # balanced tangential
dz = 0.5*len12*(cos(i1)+cos(i2))*rf
dn = 0.5*len12*(sin(i1)*cos(a1)+sin(i2)*cos(a2))*rf
de = 0.5*len12*(sin(i1)*sin(a1)+sin(i2)*sin(a2))*rf
return dz,dn,de
import numpy as np
import matplotlib.pyplot as plt
# import for 3d plot
from mpl_toolkits.mplot3d import Axes3D
# initializing 3d plot
fig = plt.figure()
ax = fig.add_subplot(111, projection = '3d')
# several data points
r = np.array([0, 14, 64, 114])
# get lengths of the separate segments
r[1:] = r[1:] - r[:-1]
phi = np.array([255.6, 255.6, 261.7, 267.4])
theta = np.array([-79.5, -79.5, -79.4, -78.8])
# convert to radians
phi = phi * 2 * np.pi / 360.
# in spherical coordinates theta is measured from zenith down; you are measuring it from horizontal plane up
theta = (90. - theta) * 2 * np.pi / 360.
# get x, y, z from known formulae
x = r*np.cos(phi)*np.sin(theta)
y = r*np.sin(phi)*np.sin(theta)
z = r*np.cos(theta)
# np.cumsum is employed to gradually sum resultant vectors
ax.plot(np.cumsum(x),np.cumsum(y),np.cumsum(z))
对于500米的钻孔,可采用最小曲率法,否则位置误差会很大。在pygsi模块中实现的pygsi。示例显示了真实钻孔数据库的完整解测过程,包括化验/岩性间隔的位置,如下所示:
http://nbviewer.ipython.org/github/opengeostat/pygslib/blob/master/pygslib/Ipython_templates/demo_1.ipynb
这也展示了如何将VTK格式的钻孔导出到paraview中的lad。在
Results shown in Paraview
Cython中去测一个区间的代码如下:
将坐标转换为笛卡尔坐标并使用matplotlib打印的脚本,其中包含以下注释:
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