STUDY THE INFLUENCE OF SOIL MOISTURE AND PACKING INCREMENTAL LEVEL ON SOIL PHYSICAL AND HYDRAULIC PROPERTIES

Simple item page
dc.contributor.authorGunaratnam A
dc.contributor.authorGrafton M
dc.contributor.authorJeyakumar P
dc.contributor.authorBishop P
dc.contributor.authorDavies C
dc.contributor.authorMcCurdy M
dc.contributor.editorChristensen, C
dc.contributor.editorHorne, D
dc.contributor.editorSingh, R
dc.coverage.spatialMassey University
dc.date.issued14/07/2020
dc.description.abstractReconstructed soil packing is an alternative for monolithic soil columns in lysimeter studies. The excavated soil is packed in uniform layers to represent the natural soil conditions. Reconstructed soil packing alters the physical properties, including bulk density and porosity, thus can distort the hydraulic properties of the soil, so consistency of the method used is critical. Therefore, the selection of a suitable packing method is imperative. This preliminary study comes under the broad research programme: “developing and testing new fertilizer formulations in lysimeters”. This work was aimed to study the effect of incremental packing methods on the hydraulic properties of soil to select the best combination for testing fertilizers. The selected soil matrix for this lysimeter study was composed of 10 cm topsoil and 30 cm washed builders’ sand. For this study, four different soil packs were trialled in lysimeters with the combination of two soil moisture conditions (dry/damp and wet) and two packing depth increments (5 and 10 cm). The flow rate and saturated hydraulic conductivity were measured. Subsequently, several pore volumes of water (around 5 – 6) was allowed to pass through the soil column and the soil subsidence level was measured for each packing method. Both soil moisture condition and packing increment level have influenced the flow rate and saturated hydraulic conductivity of the soil matrix. The saturated hydraulic conductivity of the dry-5 cm, dry-10 cm, wet-5 cm and wet-10 cm packing were 3.99, 6.70, 3.56 and 6.53 cm hr- 1 , respectively. Soil subsidence was also influenced by both the soil moisture condition and increment level. The highest soil subsidence was exhibited by dry-10 cm packing (13 mm) and lowest by wet-5 cm (2 mm) (p<0.05). This preliminary study showed that both moisture condition and increment level influence the soil hydraulic property and compaction level. Further study needs to be conducted to understand the influence of soil moisture and incremental level on other physical and hydraulic properties of soil packing.
dc.format.extent? - ? (5)
dc.identifier.citation2020, pp. ? - ? (5)
dc.identifier.elements-id433268
dc.identifier.harvestedMassey_Dark
dc.identifier.urihttps://hdl.handle.net/10179/15515
dc.relation.urihttp://flrc.massey.ac.nz/workshops/20/paperlist20.htm
dc.rightsThe Author(s), Massey University
dc.sourceNutrient Management in Farmed Landscapes.
dc.subjectPacking increment, moisture level, reconstructed soil packing, soil hydraulic property, soil subsidence level.
dc.titleSTUDY THE INFLUENCE OF SOIL MOISTURE AND PACKING INCREMENTAL LEVEL ON SOIL PHYSICAL AND HYDRAULIC PROPERTIES
dc.typeconference
pubs.confidentialFALSE
pubs.finish-date16/07/2020
pubs.notesNot known
pubs.organisational-group/Massey University
pubs.organisational-group/Massey University/College of Sciences
pubs.organisational-group/Massey University/College of Sciences/School of Agriculture & Environment
pubs.start-date12/02/2020
Files
Original bundle
Now showing 1 - 1 of 1
Thumbnail Image
Name:
Paper_Gunaratnam_2020.pdf
Size:
691.38 KB
Format:
Adobe Portable Document Format
Description:
Download
Collections
Conference Papers