Conventionally, the compaction quality of filling materials suitable for earthwork is evaluated through spot detection of the density, moisture content, strength, and modulus at some discrete points
[10,53][1][11]; for instance, the sand cone method
[56][14], electromagnetic soil density gauge method
[57][15], direct heating method
[58][16], nuclear method
[59][17], and water-filling method
[60][18] are currently used for detecting the density. As moisture content go, the methods mainly include the nuclear method
[59][17], sand cone method
[56][14], and direct heating method
[58][16]. The dynamic cone penetrometer (DCP) method
[61][19] and Clegg impact soil test (CIST) method
[62][20] are used to detect strength. In terms of modulus, the lightweight deflectometer (LWD) method
[63][21], soil stiffness gauge (SSG) method
[64][22], and plate loading test (PLT) method
[65][23] are detection methods in common use. Take the sand cone method as an example—it is a commonly used test method in the subgrade, and suitable for in situ determination of the density and moisture content of fine-grained soil, sand soil, and gravel soil
[56,66][14][24]. Up to now, the sampling point detection methods have been widely used in roads, railways, airports, dams, and embankment. These methods have high detection accuracy and have become the benchmark method for other methods. However, there are the following main problems that need to be further resolved: (1) the compaction status of the entire working area cannot be effectively reflected; (2) most methods are destructive, which greatly disturbs the compaction area; (3) low efficiency and high cost severely restrict the construction schedule, reduce construction efficiency, and project economics; (4) partial methods have high requirements for operators and operation accuracy; (5) the compaction quality of the entire working area cannot be recorded in real time, and data traceability is extremely deficient.