地质学家拥有他们自己的Minecraft:如何根据所学知识构建您所不知道的



这是关于数学如何首先入侵地质学,然后IT专家如何来对所有事物进行编程并由此创建“数字地质学家”这一新职业的故事的开篇。这是一个关于随机建模与克里金法有何不同的故事。这也是尝试展示您自己如何编写第一个地质软件,并可能以某种方式改变地质和石油工程领域的尝试。



让我们计算一下那里有多少油



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Python .



Inverse distance interpolation
import numpy as np
import matplotlib.pyplot as pl

# num of data
N = 5

np.random.seed(0)

# source data
z = np.random.rand(N)
u = np.random.rand(N)

x = np.linspace(0, 1, 100)
y = np.zeros_like(x)

# norm weights
w = np.zeros_like(x)

# power
m = 2

# interpolation
for i in range(N):
    y += z[i] * 1 / np.abs(u[i] - x) ** m
    w += 1 / np.abs(u[i] - x) ** m

# normalization
y /= w

# add source data
x = np.concatenate((x, u))
y = np.concatenate((y, z))
order = x.argsort()
x = x[order]
y = y[order]

# draw graph
pl.figure()

pl.scatter(u, z)
pl.plot(x, y)

pl.show()

pl.close()




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, — Python:



Kriging interpolation
import numpy as np
import matplotlib.pyplot as pl

# num of data
N = 5

np.random.seed(0)

# source data
z = np.random.rand(N) - 0.5
u = np.random.rand(N)

x = np.linspace(0, 1, 100)
y = np.zeros_like(x)

# covariance function
def c(h):
    return np.exp(-np.abs(h ** 2 * 20.))

# covariance matrix
C = np.zeros((N, N))

for i in range(N):
    C[i, :] = c(u - u[i])

# dual kriging weights
lamda = np.linalg.solve(C, z)

# interpolation
for i in range(N):
    y += lamda[i] * c(u[i] - x)

# add source data
x = np.concatenate((x, u))
y = np.concatenate((y, z))
order = x.argsort()
x = x[order]
y = y[order]

# draw graph
pl.figure()

pl.scatter(u, z)
pl.plot(x, y)

pl.show()

pl.close()




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Libraries
from theory import probability
from numpy import linalg


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Unconditional stochastic gaussian modeling
import numpy as np
import matplotlib.pyplot as pl

np.random.seed(0)

# source data
N = 100
x = np.linspace(0, 1, 100)

# covariance function
def c(h):
    return np.exp(-np.abs(h ** 2 * 250))

# covariance matrix
C = np.zeros((N, N))

for i in range(N):
    C[i, :] = c(x - x[i])

# eigen decomposition
w, v = np.linalg.eig(C)

A = v @ np.diag(w ** 0.5)

# you can check, that C == A @ A.T

# independent normal values
zeta = np.random.randn(N)

# dependent multinormal values
Z = A @ zeta

# draw graph
pl.figure()

pl.plot(x, Z)

pl.show()

pl.close()




4.



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Conditional stochastic gaussian simulation
import numpy as np
import matplotlib.pyplot as pl

np.random.seed(3)

# source data
M = 5

# coordinates of source data
u = np.random.rand(M)

# source data
z = np.random.randn(M)

# Modeling mesh
N = 100
x = np.linspace(0, 1, N)

# covariance function
def c(h):
return np.exp(−np.abs(h ∗∗ 2250))

# covariance matrix mesh−mesh
Cyy = np.zeros ((N, N))
for i in range (N):
    Cyy[ i , : ] = c(x − x[i])

# covariance matrix mesh−data
Cyz = np.zeros ((N, M))

# covariance matrix data−data
Czz = np.zeros ((M, M))
for j in range (M):
    Cyz [:, j] = c(x − u[j])
    Czz [:, j] = c(u − u[j])

# posterior covariance
Cpost = Cyy − Cyz @ np.linalg.inv(Czz) @ Cyz.T

# lets find the posterior mean, i.e. Kriging interpolation
lamda = np.linalg.solve (Czz, z)
y = np.zeros_like(x)

# interpolation
for i in range (M):
    y += lamda[i] ∗ c(u[i] − x)

# eigen decomposition
w, v = np.linalg.eig(Cpost)
A = v @ np.diag (w ∗∗ 0.5)

# you can check, that Cpost == A@A.T

# draw graph
pl.figure()
for k in range (5):
    # independent normal values
    zeta = np.random.randn(N)
    # dependent multinormal values
    Z = A @ zeta
    pl.plot(x, Z + y, color=[(5 − k) / 5] ∗ 3)
    pl.plot(x, Z + y, color=[(5 − k) / 5] ∗ 3, label=’Stochastic realizations’)

pl.plot(x, y, ’. ’, color=’blue’, alpha=0.4, label=’Expectation(Kriging)’)
pl.scatter(u, z, color=’red ’, label=’Source data’)
pl.legend()
pl.show()
pl.close()




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