In this article, a compressive sensing-based reconstruction algorithm is applied to data acquired from a nodding multibeam Lidar system following a Lissajous-like trajectory. Multibeam Lidar systems provide 3D depth information of the environment, but the vertical resolution of these devices may be insufficient in many applications. To mitigate this issue, the Lidar can be nodded to obtain higher vertical resolution at the cost of increased scan time. Using Lissajous-like nodding trajectories allows for the trade-off between scan time and horizontal and vertical resolutions through the choice of scan parameters. These patterns also naturally subsample the imaged area. In this article, a compressive sensing-based reconstruction algorithm is applied to the data collected during a relatively fast and therefore low-resolution Lissajous-like scan. Experiments and simulations show the feasibility of this method and compare the reconstructions to those made using simple nearest-neighbor interpolation.
For autonomous robots, having range information about the environment and the objects within it is extremely useful, if not necessary, for the robot to navigate and react to its surroundings. The data can be used for localization and/or mapping in the forms of visual odometry , SLAM , and more . In recent years, Lidar has perhaps become the most widespread way to collect this information in large part due to increasing availability and falling prices as a result of their use in self-driving automobiles. While Lidar configurations come in many different forms, recent systems tend to favor multibeam arrangements, which rotate multiple beams to provide a 3D view of the scene. However, due to limitations on how closely the beams can be spaced, the vertical resolution can be still insufficient for specific applications, as the insufficient vertical resolution can cause objects to “disappear” as they pass between visibility of one beam to another. Even if seen, it is unlikely that detection by a single beam would provide sufficient information to successfully classify the object. Newer, higher resolution Lidar models partially mitigate, but do not completely overcome, this issue.
Before multibeam Lidar systems became more widely available, single-beam planar Lidar units were (and still are, in some applications) used to collect 3D depth information by placing them on a nodding or spinning platform, allowing the plane in which the Lidar scans to be rotated . Typically, these configurations are driven through a raster scan pattern in which the assembly is rotated in a stair-step pattern between scans of the Lidar. This method results in high resolution in the dimension added due to rotation, but at the expense of significantly increased scan times. In the prior work, two of the authors explored the applicability of raster scan patterns for multibeam Lidar to help solve the “disappearing” problem and how other scan trajectories, such as Lissajous-like scan patterns, can be used to provide a trade-off between scan period and resolution . While Lissajous-like scanning could replicate depth images from the raster scan to some degree, the resulting decrease in the data gathered resulted in smaller objects being more difficult to identify.
While it is often useful to trade-off some resolution for higher frequency sampling, it is typically still desirable to have the highest resolution scan possible to support detection, mapping and SLAM. Inspired by recent results of one of the authors on increasing the imaging rate in atomic force microscopy through subsampling, combined with image reconstruction algorithms to recover high resolution detail , in this paper, we explore the use of reconstruction algorithms combined with the Lissajous-like sampling pattern in an attempt to get both high speed and high resolution. The essential idea is to view a high-resolution raster scan image as a “ground truth” image that has been subsampled through the Lissajous-like scan. The final image is formed from the data using a recent optimization algorithm for sparse reconstruction of 3D depth images . This approach differs from common Lidar reconstruction methods, which infer some information about the detected objects from segmentation or classification to determine how to perform reconstruction on the Lidar data, such as in Ref. . Instead, in this work, reconstruction is performed directly on Lidar depth images using compressive sensing (CS) techniques, without performing any other processing on the data.
In this article, experimental results are presented to establish the feasibility of this method. Specifically, Lissajous-like scans that sample less than 10% of the full raster scan data can reproduce the full raster data set with high fidelity when the CS algorithm is applied. To further the advantages of this method at very low sampling levels, the experimental data are subsampled further and then used to reconstruct the full raster data with good results. The reconstructed images are compared both visually and numerically by computing the mean squared error (MSE) between the reconstructions and the ground truth image.
Lissajous-Like Patterns in Nodding Lidar
Much of the work relevant to this section was presented in Ref.  and as a result will be presented in minimal depth here. The nodding Lidar system used for this effort is shown in Fig. 1(a). The apparatus features a direct drive system for nodding the Lidar platform and is designed so the distance separation between the Lidar’s optical center and the axis of rotation is small. The Lidar used is the Velodyne VLP-16 Puck, which rotates its beams at a rate of 20 Hz, with a horizontal resolution of 900 points per scan over a full 360 deg range and a vertical resolution of 16 equally spaced beams over a 30 deg field of view, which in total produces a maximum output of 14,400 points per scan in single return modes.
Because the parameters of the Lidar are fixed, the distribution of the scan readings is determined by the choice of trajectory for the nodding motion. For a raster scan, the trajectory is a stair-step pattern, with the Lidar nodding in small angle increments between scans of the Lidar, with a trajectory spanning from some arbitrary angle −A to A. For Lissajous-like scanning, the Lidar is nodded with a triangular trajectory between −A and A with frequency ωn (we call this “Lissajous-like” because Lissajous trajectories are typically sinusoidal in both axes). Both the raster and Lissajous-like trajectories are used to create depth images in this work, with the data from a high-resolution raster scan treated as the “ground truth” and data from low-resolution Lissajous-like scans treated as downsamples of the ground truth data.
Reconstruction of Lidar Images From Subsampled Data
The goal of the reconstruction is to fill in the missing pixels in the depth image (namely, those that were not sampled) with values that depend on the measured data. Perhaps the simplest way to do this is nearest-neighbor (NN) interpolation. Such an approach can be effective if there are sufficient data, but it does not take into account any structure in the image and may therefore produce less than ideal results. An alternative approach is to leverage results from CS. CS is a joint measurement and signal-processing technique, which can produce good (or even exact) reconstructions of signals from significantly fewer measurements than the Nyquist-Shannon sampling theorem requires . At the heart of CS is the assumption of compressibility (or true sparsity) of the signal of interest, that is, when described in an appropriate basis, most of the coefficients are negligible (compressibility) or exactly zero (sparsity).
In the context of reconstruction of a depth image from the nodding Lidar scan, measurements are restricted to values of the pixels of the image that lie on the scanned path. As a result, each row in Φ consists of a single one (indicating which pixel is measured) with all other entries being zero. Thus, the measurement matrix Φ is given by extracting rows from an n × n identity matrix. This has implications for a property known as the mutual coherence , generally implying that reconstructions from the data sampled by Φ from solving Eq. (3) will not be exact and in general may have a large error. The metric of mutual coherence is in general improved by using random sampling, and experience in many applications has shown good performance (see, e.g., Refs. [11,12]).
As it turns out, in structured environments such as one finds in indoor environments, the depth profile is often well described as consisting of many planar regions connected by a few “edges.” The sparsity of the data, then, is not with respect to a particular sparsity basis, but rather with respect to these edges. This case was first considered in Ref.  where a reconstruction algorithm was created using a cosparsity model. We give a brief description here.
Experimental Imaging and Reconstruction
In this work, an indoor and an outdoor space were imaged by the Lidar. The Lidar followed a nodding trajectory of , which provided a sufficient field of view to visualize the relevant objects in the space (but not things considered unnecessary, such as the ceiling of the indoor space). The spaces are first scanned by the Lidar undergoing a raster scan trajectory with a period of 10 s. Then, the spaces are scanned by the Lidar with Lissajous-like trajectories with periods of 1 s and 0.25 s. These Lissajous-like scans can be treated as “subsampled” versions of the raster scan, which is treated as the ground truth, with downsampling percentages of and , respectively.
Figure 2 shows the indoor space imaged by a color camera and the nodding Lidar. A panoramic color image is presented in Fig. 2(a) to familiarize the reader with the space. The raster scan is shown in Fig. 2(b), and the 1-s and 0.25-s Lissajous-like scans are shown in Figs. 2(c) and 2(d), respectively. The data from the Lidar scans are displayed as depth images, with closer objects being whiter and regions where there are no data from the scan showing as black. Note that, because of how the grid is generated for the depth images, the downsampling percentages of the Lissajous-like scans do not correspond to the percentage of populated pixels in the depth images. This is because of cases where multiple points are associated with the same pixel, commonly along the sides of the scan where measurements are more clustered.
Reconstructions of the indoor Lidar data from the Lissajous-like scan in Fig. 2(d) are shown in Fig. 2(e) for the NN interpolation and Fig. 2(f) for the CS-based reconstruction. Both the NN- and CS-based reconstructions are visually quite good. While there are only minor differences between them, in general, edges are (slightly) crisper in the CS-based reconstruction, especially on linear edges like the pillars at the middle and far right of the images.
To explore performance at extremely low sampling, the 2.5% Lissajous-like scan data were further subsampled by discarding some of the data. This was done in two ways: first by keeping only every 10th sample (thus regularly subsampling) and second by randomly selecting of the sample points, both resulting in a total subsampling of from the raster scan. (In practice, of course, one would not discard data but rather choose to only acquire the limited set.) The NN- and CS-based reconstructions were performed again on these downsamples.
To compare all the reconstructions, we consider the focus area bound by a red rectangle in Fig. 2(b) containing a workbench and a chair. Each reconstruction of this region from the Lissajous-like scan, as well as from the downsamples of the Lissajous-like scan, is shown in Fig. 3. Qualitatively speaking, the appearance of the bench and the chair seems to have more detail, but are more prone to noise around the edges, in the reconstructions in Fig. 3 (left column). In the middle and right columns of Fig. 3, both the nearest neighbor and CS reconstructions of the are remarkably good given the extremely low sampling, but clearly are degraded relative to the reconstructions from the data. For the reconstructions, the same relationship between the CS and NN reconstruction is observed as earlier: the edges tend be slightly more crisp in the CS reconstruction. In addition, for the CS reconstructions, the randomly subsampled image is visually superior to the regularly subsampled version despite the same level of subsampling. Interestingly, the nearest-neighbor interpolation seems to have darkened the randomly subsampled scan during the reconstruction process, while the compressive sensing-based method retained the original intensity (and hence, depth values).
Figure 4 shows the outdoor space imaged by a color camera and depth images from the raster and Lissajous-like scans. While the full reconstruction results are not shown here, the reconstructions of the subsampled data behave similarly as the indoor case, in that both algorithms have comparable performance but the CS reconstruction tends to have sharper edges. The reconstructions for the region highlighted in Fig. 4(b) are shown in Fig. 5. This is an especially difficult region for the reconstruction techniques to resolve as the trees are very close to each other but not touching. As before, the NN and CS techniques applied to the Lissajous-like scan data, shown in Fig. 5 (left column), have comparable performance although the edges of the trees are slightly more distinct in the CS reconstruction. Further, downsampling in Fig. 5 (middle and right columns) significantly degrades the reconstruction performance, with the trees being merged into one object in both reconstructions of the regularly subsampled data. When reconstructing the randomly subsampled data, the CS method almost manages to resolve the two middle trees as separate objects, while the NN interpolation resolves them into a single shape with a few holes.
The values of MSE′ are presented in Table 1 for reconstructions from the and data. The MSE′ results are shown not only for the full images (indoor full, outdoor full) but also for the regions of the images highlighted in Figs. 2(b) and 4(a). Both reconstructions from the (nonsubsampled) scan have comparable performance, except the outdoor trees subsection, in which the CS technique resolved the edges of the trees significantly better than NN for that particular region. The results for the reconstructions start to diverge when the scans are subsampled further. When the data are regularly subsampled, the nearest-neighbor interpolation outperforms the compressive sensing-based reconstruction by a small margin (5–10%) indoors and by a smaller margin outdoors. However, when the data are randomly subsampled instead, the compressive sensing-based reconstruction outperforms the nearest-neighbor interpolation by a large margin (25–35%) indoors, and a smaller performance improvement () outdoors for the trees region outdoors, but not for the full outdoor image.
In general, it appears that the CS reconstruction has comparable or better performance than the NN technique for indoor environments, with significant improvement when the data are randomly sampled. The CS reconstruction also typically appears to have better performance in regions with straight edges, such as the pillars in the indoor space or the highlighted region of the outdoor space. This is likely a result of the choice of convolutional kernels, which were designed to fit the data profile while minimizing the number of depth changes in the horizontal, vertical, and diagonal directions. This indicates that perhaps appropriate kernels could be designed for other environments with known, but structure that is more complicated than simple planes and straight lines.
In all cases but the full outdoor image, the CS technique performed significantly better on randomly subsampled data than regularly subsampled data, highlighting that randomness is important in subsampling. In fact, it has been shown that random sampling matrices are maximally incoherent with any fixed sensing matrix  and should thus be expected to outperform deterministic sampling in the general setting.
The use of CS reconstruction algorithms for Lissajous-like nodding Lidar was presented. This method allows for very small amounts of data and thus very small data collection times to produce high fidelity depth data. Experimental and simulation results show the feasibility of this approach in both indoor and outdoor scenarios.
The work of Sathishchandra and Andersson was supported in part by the NSF through CMMI-1562031. The work of Benson and Clayton was supported in part by the NSF through OISE-1658696.