2021
DOI: 10.1007/s12517-021-08263-0
|View full text |Cite
|
Sign up to set email alerts
|

Techniques for ground-based soil moisture measurement: a detailed overview

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1

Citation Types

0
3
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
8
1

Relationship

0
9

Authors

Journals

citations
Cited by 11 publications
(5 citation statements)
references
References 247 publications
0
3
0
Order By: Relevance
“…Ground-coupled GPR Time Depth of reflector 450; 900 225/450/900 [108] Ground wave method Ground-coupled GPR (or surface GPR) Time ≤30 cm (Penetrating depth of ground wave in soil) 225/450/900 [121] AEA method Ground-coupled GPR Amplitude and Waveform ≤30 cm 250/500 [1,122] FWI method --All attributes of recorded signal ~2 cm 1000~2000 [123] Frequency shift method Ground-coupled GPR Energy and phase etc. 10 cm 600 [2] Borehole GPR method Borehole GPR Time Maximum distance between receiver and transmitter 100; 250 [119] When the dielectric permittivity is converted from GPR to volumetric SWC, relationships must be used.…”
Section: Reflected Wave Methodsmentioning
confidence: 99%
“…Ground-coupled GPR Time Depth of reflector 450; 900 225/450/900 [108] Ground wave method Ground-coupled GPR (or surface GPR) Time ≤30 cm (Penetrating depth of ground wave in soil) 225/450/900 [121] AEA method Ground-coupled GPR Amplitude and Waveform ≤30 cm 250/500 [1,122] FWI method --All attributes of recorded signal ~2 cm 1000~2000 [123] Frequency shift method Ground-coupled GPR Energy and phase etc. 10 cm 600 [2] Borehole GPR method Borehole GPR Time Maximum distance between receiver and transmitter 100; 250 [119] When the dielectric permittivity is converted from GPR to volumetric SWC, relationships must be used.…”
Section: Reflected Wave Methodsmentioning
confidence: 99%
“…Moreover, soil moisture dynamics also play a key role in predicting the potential impact of weather events on, e.g., fires, floods, and landslides, and on soil productivity and ecosystems as described in [4]. Despite its importance, soil moisture is one of the least understood and most difficult variables to measure in the field of soil hydrology [5]. Moreover, vegetation plays a fundamental role in soil moisture at different spatial and temporal scales, as plants extract water from the soil and influence water pathways and flows [6,7].…”
Section: Introductionmentioning
confidence: 99%
“…The gravimetric method is the direct and natural way to measure SM. However, it is very labor-intensive and time-consuming, although it accurately gives ground truth data of soil moisture content [4], [5]. All other SM measurement technique comes under the indirect measurement method, indirect because they use the change in the internal property of the sensory system as a proxy for soil water content (SWC).…”
Section: Introductionmentioning
confidence: 99%
“…In the ground contact type sensor category, timedomain reflectometry, time-domain transmission, frequency domain reflectometry, neutron probe, electrical resistance, electromagnetic sensors, and tensiometers are widely used [5]- [9]. However, due to the setup cost and bulkiness, these methods are less preferred for soil moisture monitoring [4], [5], [10], [11].…”
Section: Introductionmentioning
confidence: 99%