示例#1
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    def rpp_t(self, dt):

        if self.domain == 'time':
            if dt == self.dz:
                return self.rpp
            else:
                raise Exception('sampling mismatch')

        vpt = depth_to_time(self.vp, self.vp, self.dz, dt)
        times = np.arange(vpt.shape[0]) * dt
        vst = depth_to_time(self.vs, self.vp, self.dz, times)
        rhot = depth_to_time(self.rho, self.vp, self.dz, times)

        rpp = reflectivity_array(vpt, vst, rhot, self.theta)
        return rpp
示例#2
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    def test_recip(self):
        data = np.zeros((100, 100))
        vmodel = np.zeros((100, 100))

        data[0:50, :] += 100.0
        data[50:, :] += 200.0

        vmodel[0:50, :] += 1500.0
        vmodel[50:, :] += 1800.0

        dt = 0.001
        dz = 1.

        out1 = depth_to_time(data, vmodel, dz, dt)
        v2 = depth_to_time(vmodel, vmodel, dz, dt)
        out2 = time_to_depth(out1, v2, dt, dz)
示例#3
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    def test_recip(self):
        data = np.zeros((100, 100))
        vmodel = np.zeros((100, 100))

        data[0:50, :] += 100.0
        data[50:, :] += 200.0

        vmodel[0:50, :] += 1500.0
        vmodel[50:, :] += 1800.0

        dt = 0.001
        dz = 1.

        out1 = depth_to_time(data, vmodel, dz, dt)
        v2 = depth_to_time(vmodel, vmodel, dz, dt)
        out2 = time_to_depth(out1, v2, dt, dz)
示例#4
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    def rpp_t(self, dt):

        if self.domain == 'time':
            if dt == self.dz:
                return self.rpp
            else:
                raise Exception('sampling mismatch')
            
        
        vpt = depth_to_time(self.vp, self.vp, self.dz, dt)
        times = np.arange(vpt.shape[0]) * dt
        vst = depth_to_time(self.vs, self.vp, self.dz, times)
        rhot = depth_to_time(self.rho, self.vp, self.dz, times)

        rpp = reflectivity_array(vpt, vst, rhot, self.theta)
        return rpp
示例#5
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    def test_depthtotime(self):
        data = np.zeros((100, 100))
        vmodel = np.zeros((100, 100))

        data[0:50, :] += 100.0
        data[50:, :] += 200.0

        vmodel[0:50, :] += 1500.0
        vmodel[50:, :] += 3000.0

        dt = 0.001
        dz = 1.0

        face_change = np.floor(((49 * dz) / 1500.0) / dt)

        output = depth_to_time(data, vmodel, dz, dt, twt=False)

        self.assertTrue((output[face_change + 1, 50] - output[face_change, 50]) == 100)
示例#6
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    def test_depthtotime(self):
        data = np.zeros((100, 100))
        vmodel = np.zeros((100, 100))

        data[0:50, :] += 100.0
        data[50:, :] += 200.0

        vmodel[0:50, :] += 1500.0
        vmodel[50:, :] += 3000.0

        dt = 0.001
        dz = 1.0

        face_change = int(np.floor(((49 * dz) / 1500.0) / dt))

        output = depth_to_time(data, vmodel, dz, dt, twt=False)

        self.assertTrue((output[face_change + 1, 50] -
                         output[face_change, 50]) == 100)
示例#7
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    def depth2time(self, dt, samples=None):

        if self.units == 'time':
            raise ValueError

        vp_data = self.vp_data(samples=samples)
        data = self.get_data(samples=samples)

        indices = np.array([np.arange(vp_data.shape[0])
                            for i in range(vp_data.shape[1])])\
                    .transpose()

        dz = self.depth / data.shape[0]

        time_index = depth_to_time(indices, vp_data, dz, dt).astype(int)

        self.image = np.asarray([data[time_index[:, i], i, :]
                                 for i in range(data.shape[1])])\
                       .transpose(1, 0, 2)
示例#8
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    def depth2time(self, dt, samples=None):

        if self.units == 'time':
            raise ValueError

        vp_data = self.vp_data(samples=samples)
        data = self.get_data(samples=samples)

        indices = np.array([np.arange(vp_data.shape[0])
                            for i in range(vp_data.shape[1])])\
                    .transpose()

        dz = self.depth / data.shape[0]

        time_index = depth_to_time(indices, vp_data,
                                   dz, dt).astype(int)

        self.image = np.asarray([data[time_index[:, i], i, :]
                                 for i in range(data.shape[1])])\
                       .transpose(1, 0, 2)
示例#9
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文件: model.py 项目: praffiah/jeepr
    def to_time(self, v=None, dt=1e-12):
        """
        Convert model to time domain.

        Args:
            v (ndarray): Interval velocities. Must be same shape as model. If
                None, then the model's own permittivities are used.
            dt (float): The new time step or sampling interval, in seconds.

        Returns:
            Model. The time-converted model, as a jeepr.Model instance.
        """
        if self.domain != 'depth':
            raise ModelError('You can only time-convert a depth model.')
        params = copy.deepcopy(self.__dict__)
        if v is None:
            v = self.velocity
        arr = depth_to_time(self, v, dz=self.dz, dt=dt)
        basis = utils.srange(0, dt, arr.shape[0])
        params['domain'] = 'time'
        params['dz'] = 0
        params['dt'] = dt
        return Model(arr, params), basis
示例#10
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def run_script(json_payload):

    # parse json
    fs_model = FluidSub1D.from_json(json_payload["earth_model"])
    seismic = Seismic.from_json(json_payload["seismic"])

    # extract rock properties
    vp, vs, rho = (fs_model.vp, fs_model.vs, fs_model.rho)
    vp_sub, vs_sub, rho_sub = fs_model.smith_sub()

    # convert to time
    dt = seismic.dt
    dz = fs_model.dz
    z = fs_model.z

    # use indices so we only run the algorithm once
    index = np.arange(vp.size, dtype=int)
    t_index = depth_to_time(index, vp, dz, dt).astype(int)
    sub_t_index = depth_to_time(index, vp_sub, dz, dt).astype(int)
    vp_t, vs_t, rho_t = (vp[t_index], vs[t_index], rho[t_index])
    vp_sub_t, vs_sub_t, rho_sub_t = (vp_sub[sub_t_index], vs_sub[sub_t_index],
                                     rho_sub[sub_t_index])

    # calculate reflectivities
    rpp = np.nan_to_num(
        np.array([
            zoep(vp_t[:-1], vs_t[:-1], rho_t[:-1], vp_t[1:], vs_t[1:],
                 rho_t[1:], float(theta)) for theta in seismic.theta[::-1]
        ]).T)

    rpp_sub = np.nan_to_num(
        np.array([
            zoep(vp_sub_t[:-1], vs_sub_t[:-1],
                 rho_sub_t[:-1], vp_sub_t[1:], vs_sub_t[1:], rho_sub_t[1:],
                 float(theta)) for theta in seismic.theta[::-1]
        ]).T)

    # trim to be the same size
    n = min(rpp.shape[0], rpp_sub.shape[0])
    rpp = rpp[:n, :]
    rpp_sub = rpp_sub[:n, :]
    t = np.arange(n) * dt

    # create synthetic seismic
    traces = np.squeeze(do_convolve(seismic.src, rpp[:, np.newaxis, :]))
    sub_traces = np.squeeze(do_convolve(seismic.src, rpp_sub[:,
                                                             np.newaxis, :]))

    output = {
        "vp":
        vp.tolist(),
        "vs":
        vs.tolist(),
        "rho":
        rho.tolist(),
        "vp_sub":
        vp_sub.tolist(),
        "vs_sub":
        vs_sub.tolist(),
        "rho_sub":
        rho_sub.tolist(),
        "synth":
        np.nan_to_num(traces).T.tolist(),
        "synth_sub":
        np.nan_to_num(sub_traces).T.tolist(),
        "theta":
        seismic.theta,
        "rpp":
        rpp[:, 0].tolist(),
        "rpp_sub":
        rpp_sub[:, 0].tolist(),
        "t_lim": [float(np.amin(t)), float(np.amax(t))],
        "z_lim": [float(np.amin(z)), float(np.amax(z))],
        "vp_lim": [float(np.amin((vp, vp_sub))),
                   float(np.amax((vp, vp_sub)))],
        "vs_lim": [float(np.amin((vs, vs_sub))),
                   float(np.amax((vs, vs_sub)))],
        "rho_lim":
        [float(np.amin((rho, rho_sub))),
         float(np.amax((rho, rho_sub)))],
        "rpp_lim":
        [float(np.amin((rpp, rpp_sub))),
         float(np.amax((rpp, rpp_sub)))],
        "synth_lim": [
            float(np.amin((traces, sub_traces))),
            float(np.amax((traces, sub_traces)))
        ],
        "dt":
        dt,
        "dz":
        dz
    }

    return output
示例#11
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def run_script(json_payload):

    # parse json
    fs_model = FluidSub1D.from_json(json_payload["earth_model"])
    seismic = Seismic.from_json(json_payload["seismic"])

    # extract rock properties
    vp, vs, rho = (fs_model.vp, fs_model.vs, fs_model.rho)
    vp_sub, vs_sub, rho_sub = fs_model.smith_sub()

    # convert to time
    dt = seismic.dt
    dz = fs_model.dz
    z = fs_model.z
    
    # use indices so we only run the algorithm once
    index = np.arange(vp.size, dtype=int)
    t_index = depth_to_time(index, vp, dz, dt).astype(int)
    sub_t_index = depth_to_time(index, vp_sub, dz, dt).astype(int)
    vp_t, vs_t, rho_t = (vp[t_index], vs[t_index], rho[t_index])
    vp_sub_t, vs_sub_t, rho_sub_t = (vp_sub[sub_t_index],
                                     vs_sub[sub_t_index],
                                     rho_sub[sub_t_index])

    # calculate reflectivities
    rpp = np.nan_to_num(np.array([zoep(vp_t[:-1], vs_t[:-1], rho_t[:-1],
                                       vp_t[1:], vs_t[1:], rho_t[1:],
                                       float(theta))
                                  for theta in seismic.theta[::-1]]).T)

    rpp_sub = np.nan_to_num(np.array([zoep(vp_sub_t[:-1], vs_sub_t[:-1],
                                           rho_sub_t[:-1],
                                           vp_sub_t[1:], vs_sub_t[1:],
                                           rho_sub_t[1:], float(theta))
                                      for theta in seismic.theta[::-1]]).T)

    # trim to be the same size
    n = min(rpp.shape[0], rpp_sub.shape[0])
    rpp = rpp[:n, :]
    rpp_sub = rpp_sub[:n, :]
    t = np.arange(n) * dt

    # create synthetic seismic
    traces = np.squeeze(do_convolve(seismic.src, rpp[:, np.newaxis, :]))
    sub_traces = np.squeeze(do_convolve(seismic.src,
                                        rpp_sub[:, np.newaxis, :]))

    output = {"vp": vp.tolist(), "vs": vs.tolist(),
              "rho": rho.tolist(), "vp_sub": vp_sub.tolist(),
              "vs_sub": vs_sub.tolist(), "rho_sub": rho_sub.tolist(),
              "synth": np.nan_to_num(traces).T.tolist(),
              "synth_sub": np.nan_to_num(sub_traces).T.tolist(),
              "theta": seismic.theta,
              "rpp": rpp[:, 0].tolist(),
              "rpp_sub": rpp_sub[:, 0].tolist(),
              "t_lim": [float(np.amin(t)), float(np.amax(t))],
              "z_lim": [float(np.amin(z)), float(np.amax(z))],
              "vp_lim": [float(np.amin((vp, vp_sub))),
                         float(np.amax((vp, vp_sub)))],
              "vs_lim": [float(np.amin((vs, vs_sub))),
                         float(np.amax((vs, vs_sub)))],
              "rho_lim": [float(np.amin((rho, rho_sub))),
                          float(np.amax((rho, rho_sub)))],
              "rpp_lim": [float(np.amin((rpp, rpp_sub))),
                          float(np.amax((rpp, rpp_sub)))],
              "synth_lim": [float(np.amin((traces, sub_traces))),
                            float(np.amax((traces, sub_traces)))],
              "dt": dt,
              "dz": dz}

    return output