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Larisa Golovko, PhD
Landviser LLC and RiceTec Inc,
Houston, TX
Presented at
Agricultural Geophysics and Material Properties. Symposium on
the Application of Geophysics to Engineering and Environmental
Problems 2015: pp. 1-11.
https://doi.org/10.4133/SAGEEP.28-001
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
3
4
10 Ohm m =1 dS/m = 1 mS/cm =
1 mmho/cm = 640 ppm =
640 mg/L= 0.64 g/L=0.064%.
Veris
USDA Salinity Lab
AEMP-14, from KB Electrometry (Russia)
Quick EM method of EC mapping
down to 10 m, 14 frequencies.
Other EM Equipment by Dualem,
Geonics, GF Instruments, etc.
7
 Fits in shirt pocket
 Runs all season from standard
9V battery
 Measures EC/ER in irrigation
water, saturated soil paste
as well as in the field soils
from 2 cm to ~20 m depth
8
 No calibration – EC output
calibrated once for each probe
size.
 No GPS integration – no wait for
satellite fix
 Push one button – get EC value
in 4 seconds!
 Stores 1000 EC values – can be
merged with concurrently taken
GPS data to produce quick
maps.
9
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
.
 Planted hybrids along with
varietal checks at the farm.
 Variable readings 300 – 1700
ppm in test area
0
1000
2000
3000
4000
5000
6000
7000
8000
9000
EP1122
EP1122
CLXL8
CLXL8
CL161
CL161
CL131
CL131
XP730
XP730
XP729
XP729
Rice yield, lb/acre Soil salinity at planting, ppm Soil salinity at harvest, ppm
No salt 294 ppm
0.5 gm/kg 378 ppm
1.0 gm/kg 302 ppm
1.5 gm/kg 581 ppm
2.0 gm/kg 721 ppm
2.3 gm/kg 1043 ppm
LA soil (check) 1570 ppm
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
25
35
45
55
65
75
85
95
%ofhealthyplants
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
 Storm surge brings in salt
water
 Drought leaves it in place
 High pumping cost
reduces options for
flushing soil
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
 Spatial variability
 Temporal
variability
 Many samples
are needed to
characterize a
single field.
 management practices
 water table depths
 soil properties
 evapotranspiration rates
 rainfalls
 salinity levels of
groundwater
 hydrogeological
conditions
 Speed of
turn-over
 Units
 Techniques –
results non-
comparable
between
different labs
1000 umho/cm = 1 dS/m = 10 Ohm m = 1/ 640 ppm = 0.64 g/L =
0.064% = 45.7 grains per gallon
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
y = 0.1225x + 2.7372
R² = 0.5156
0
1
2
3
4
5
6
7
8
0 5 10 15 20 25 30
FieldERin1',Ohmm
TAMU Soil Extract conductivity, Ohm m
Resistivity of soil solution vs in-situ values
• 910 acres research farm
• 426 points ER measured at
1’ and 2’ depth
• 2 days, 2 LandMappers, 3
people, AT vehicle (mule)
 More dense measurements
in problem fields
 Cross-scanning other fields
 Collecting samples from
areas of very low/high
resistivity
Top: bad, deep: non-salty
Top: bad, deep: salty
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
 Good soil EC in top 30 cm < 1.5 dS/m (ER > 6
Ohm m) measured in flooded or “mud” conditions
 EC of irrigation water <1 dS/m (ER > 10 Ohm m) –
no yield reduction
 EC of irrigation water 1-3 dS/m (ER=3-10 Ohm m)
– yield reduction up to 50%
 On marginally salty soils/water:
 delay permanent flood - use several flushing with fresh
water instead, reduce N fertilizer, apply some gypsum on
sodic soil pre-season, consider switching to other crops or
rice hybrids
36
OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER
 USA Farmers (James Gentz, Jim White, David Murrel, Mr. Saltzman, Mr.
Goulding).
 RiceTec Inc. (Derrol Grimes, Robert Miller, Mark Spilman, Jose Plaza, Jaime
Suarez) & Helena Chemicals (Ronnie Melancor)
 Russian Visiting Scientists (Alexey Rusakov, Anatoly Pozdnyakov)
 Indonesian STEM Oil and Gas University, Cepu, Central Java)
www.landviser.net

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OPTIMIZING IN-SITU SOIL SALINITY MAPPING WITH LANDMAPPER

  • 1. Larisa Golovko, PhD Landviser LLC and RiceTec Inc, Houston, TX Presented at Agricultural Geophysics and Material Properties. Symposium on the Application of Geophysics to Engineering and Environmental Problems 2015: pp. 1-11. https://doi.org/10.4133/SAGEEP.28-001
  • 3. 3
  • 4. 4 10 Ohm m =1 dS/m = 1 mS/cm = 1 mmho/cm = 640 ppm = 640 mg/L= 0.64 g/L=0.064%.
  • 6. AEMP-14, from KB Electrometry (Russia) Quick EM method of EC mapping down to 10 m, 14 frequencies. Other EM Equipment by Dualem, Geonics, GF Instruments, etc.
  • 7. 7
  • 8.  Fits in shirt pocket  Runs all season from standard 9V battery  Measures EC/ER in irrigation water, saturated soil paste as well as in the field soils from 2 cm to ~20 m depth 8
  • 9.  No calibration – EC output calibrated once for each probe size.  No GPS integration – no wait for satellite fix  Push one button – get EC value in 4 seconds!  Stores 1000 EC values – can be merged with concurrently taken GPS data to produce quick maps. 9
  • 14. .
  • 15.  Planted hybrids along with varietal checks at the farm.  Variable readings 300 – 1700 ppm in test area
  • 17. No salt 294 ppm 0.5 gm/kg 378 ppm 1.0 gm/kg 302 ppm 1.5 gm/kg 581 ppm 2.0 gm/kg 721 ppm 2.3 gm/kg 1043 ppm LA soil (check) 1570 ppm
  • 24.  Storm surge brings in salt water  Drought leaves it in place  High pumping cost reduces options for flushing soil
  • 26.  Spatial variability  Temporal variability  Many samples are needed to characterize a single field.
  • 27.  management practices  water table depths  soil properties  evapotranspiration rates  rainfalls  salinity levels of groundwater  hydrogeological conditions
  • 28.  Speed of turn-over  Units  Techniques – results non- comparable between different labs 1000 umho/cm = 1 dS/m = 10 Ohm m = 1/ 640 ppm = 0.64 g/L = 0.064% = 45.7 grains per gallon
  • 30. y = 0.1225x + 2.7372 R² = 0.5156 0 1 2 3 4 5 6 7 8 0 5 10 15 20 25 30 FieldERin1',Ohmm TAMU Soil Extract conductivity, Ohm m Resistivity of soil solution vs in-situ values
  • 31. • 910 acres research farm • 426 points ER measured at 1’ and 2’ depth • 2 days, 2 LandMappers, 3 people, AT vehicle (mule)
  • 32.  More dense measurements in problem fields  Cross-scanning other fields  Collecting samples from areas of very low/high resistivity
  • 33. Top: bad, deep: non-salty Top: bad, deep: salty
  • 36.  Good soil EC in top 30 cm < 1.5 dS/m (ER > 6 Ohm m) measured in flooded or “mud” conditions  EC of irrigation water <1 dS/m (ER > 10 Ohm m) – no yield reduction  EC of irrigation water 1-3 dS/m (ER=3-10 Ohm m) – yield reduction up to 50%  On marginally salty soils/water:  delay permanent flood - use several flushing with fresh water instead, reduce N fertilizer, apply some gypsum on sodic soil pre-season, consider switching to other crops or rice hybrids 36
  • 38.  USA Farmers (James Gentz, Jim White, David Murrel, Mr. Saltzman, Mr. Goulding).  RiceTec Inc. (Derrol Grimes, Robert Miller, Mark Spilman, Jose Plaza, Jaime Suarez) & Helena Chemicals (Ronnie Melancor)  Russian Visiting Scientists (Alexey Rusakov, Anatoly Pozdnyakov)  Indonesian STEM Oil and Gas University, Cepu, Central Java) www.landviser.net