Estimation of vineyard soil structure and preferential flow using dye tracer, X-ray tomography, and numerical simulations

Filipović, Vilim; Defterdarović, Jasmina; Šimůnek, Jiřı́; Filipović, Lana; Ondrašek, Gabrijel; Romić, Davor; Bogunović, Igor; Mustać, Ivan; Ćurić, Josip; Kodešová, Radka

doi:10.1016/j.geoderma.2020.114699

Cited by 35 publications

(30 citation statements)

References 61 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…However, CT only visualised soil pores architecture with a static state (Lucas et al, 2019). The implementation of CT alone could not be sufficient to investigate water and solute transport processes (Filipović et al, 2020). In our study, preferential flow indices (LI, MID, and PFF) were positively correlated with the number of macropores and macroporosity ( p < 0.05; Table 4).…”

Section: Discussionmentioning

confidence: 99%

“…The CT method provided more information about the characteristics and continuity of macropores (Filipovi c et al, 2020). Lucas et al (2019) used the CT method to visualise soil pore architecture affected by plant roots.…”

Section: Introductionmentioning

confidence: 99%

“…Macropores are large soil voids and pathways, for example, root channels, and connected large pores can permit preferential flow through the soil profile (Hendrickx & Flury, 2001; Jarvis, 2020). The CT method provided more information about the characteristics and continuity of macropores (Filipović et al, 2020). Lucas et al (2019) used the CT method to visualise soil pore architecture affected by plant roots.…”

Section: Introductionmentioning

confidence: 99%

See 2 more Smart Citations

Soil macroporosity and water flow in the root zone of oases in hyper‐arid regions

Zhang

Jia

Zhao

et al. 2022

European J Soil Science

View full text Add to dashboard Cite

The characteristics of soil macropores and water infiltration are closely connected to the growth of plant roots and their root zone environment. However, it is unclear how the root zone environment of oasis farmlands regulates the development of soil macropores and water flow in hyper‐arid regions. The objective of this study was to investigate soil macropores and their effect on water flow under irrigated oasis farmlands using a combination of X‐ray computed tomography (CT) and dye tracer. It was hypothesized that the integration of CT and dye tracer could clearly reveal preferential flow through biopores and large pores of oasis soils. A helical medical CT scanner was used to quantify more information about soil macropores in the root zone, along with an in situ single‐ring dye infiltration experiment to reveal water flow in three different oasis farmlands (piedmont oasis farmland, marginal oasis farmland, and old oasis farmland). Soil macroporosity was 0.44% under crop rows, while soil macroporosity in the interrows was only 0.30% across the oasis farmlands. Biopores contributed 73% of the volume of the total macropores under crop rows. The stable infiltration rate in the interrows was 0.3 mm min−1, which was significantly (p < 0.05) less than that under crop rows (0.7 mm min−1). Water flow under crop rows were mainly transported in biopores and large pores. The contribution of macropores to preferential flow under crop rows was 4.8 times larger than interrows. The integration of CT and dye tracer was a more holistic technique, which adequately revealed that oases had preferential flow affected by biopores and large pores, resulting in higher solute and contaminant transport. Key Points Soil macropores and preferential flow affected by crop roots were investigated in hyper‐arid regions. The integration of CT and dye tracer adequately identified preferential flowpaths of oasis soils. Biopores were larger under crop rows than interrows. Preferential flow transported in biopores and large soil pores under crop rows.

show abstract

Section: Discussionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 1 more Smart Citation

Soil macroporosity and water flow in the root zone of oases in hyper‐arid regions

Zhang

Jia

Zhao

et al. 2022

European J Soil Science

View full text Add to dashboard Cite

show abstract

“…For the extraction of in‐situ earthworm burrow morphology, the major methods include the following: liquid latex and resin infusion (Li et al., 2019; Li et al., 2018), and dye tracing (Filipović et al., 2020). However, each method has limitations, and none are used widely.…”

Section: Introductionmentioning

confidence: 99%

“…Filipović et al. (2020) suggested that the adsorption of dyes on pore walls led to overestimation of flow. Kodešová et al.…”

Section: Introductionmentioning

confidence: 99%

In‐situ tin casting combined with three‐dimensional scanner to quantify anecic earthworm burrows

Zhang

Zeng

Wen

et al. 2022

Vadose Zone Journal

View full text Add to dashboard Cite

Earthworms (Lumbricus terrestris) play a critical role in soil ecosystems. Analyzing the spatial structure of earthworm burrows is important to understand their effect on water flow and solute transport. The aim of this study was to quantitatively characterize structural characteristics (cross-sectional area [A], circularity [C], diameter [D], actual length [L t ], tortuosity [τ]) of anecic earthworm burrows that were open and connected at the soil surface at two sites of different tillage treatments (no-till at Lu Yuan [LY] and rotary tillage at Shang Zhuang [SZ]) by combining a new insitu tin casting method with three-dimensional (3D) laser scanning technology. The cross-sections of anecic earthworm burrows were almost circular, and the C values were significantly negatively correlated with D and A. Statistically, there were no significant differences in the τ values (1.143 ± 0.082 vs. 1.133 ± 0.108) of anecic earthworm burrows at LY and SZ, but D (6.456 ± 1.585 mm) and A (36.929 ± 21.656 mm 2 ) of anecic earthworm burrows at LY were significantly larger than D (3.449 ± 0.531 mm) and A (9.786 ± 2.885 mm 2 ) at SZ. Our study showed that burrow structures at two different sites differed from each other. Soil tillage methods, soil texture, and soil organic matter content at the two sites could have affected earthworm species composition, variation of earthworm size and the morphology of burrows. The method used in this research enabled us to adequately assess the spatial structure of anecic earthworm burrows in the field with a limited budget.

show abstract

Dye solution experiments for determining solute transport behaviour in degraded wetland soils of the Yellow River Delta

et al. 2022

View full text Add to dashboard Cite

Solute transport behaviour can indicate the efficiency of eco-hydrological responses.However, this behaviour has not been consider for use in assessing the health of wetland ecosystems. We assessed solute transport behaviour in degraded wetland soils using 72 undisturbed soil columns located in Robinia pseudoacacia (tree) and Tamarix chinensis (bush) communities. Soil column tracer experiments were conducted under the same initial and boundary conditions using Brilliant Blue FCF as a conservative tracer. Solute transport behaviour at a soil column scale was described by four measures: steady infiltration rate of effluents, concentration of effluents, dye staining patterns and cumulative effluents leaching. Numerical modelling by the dualpermeability model in HYDRUS-1D was used to simulate the proportion of cumulative effluents leaching from soil macropores. These data showed that steady infiltration rate of effluents at the tree site decreased with increasing soil depth (5.742, 0.716, 0.657, and 0.458 ml/min) but at the bush site first increased and then subsequently decreased with increasing soil depth (0.336, 0.548, 0.974 and 0.379 ml/min).The concentration of effluents at the tree site (0.583, 0.149, 0.147 and 0.067 g/L) and the bush site (0.281, 0.109, 0.161 and 0.053 g/L) decreased nonlinearly with increasing soil depth. Dye staining patterns were significantly different between different soil locations. The largest dark blue staining domains were from 0 to 10 cm soil depths at the tree site and 20-40 cm depths at the bush site. The proportion of cumulative effluents leaching from soil macropores ranged from 37.6% to 61.1% at the tree site and ranged from 0% to 99.9% at the bush site. Understanding the solute transport behaviour in the Yellow River Delta is the first step towards the restoration of degraded wetlands.

show abstract

Estimation of vineyard soil structure and preferential flow using dye tracer, X-ray tomography, and numerical simulations

Cited by 35 publications

References 61 publications

Soil macroporosity and water flow in the root zone of oases in hyper‐arid regions

Soil macroporosity and water flow in the root zone of oases in hyper‐arid regions

In‐situ tin casting combined with three‐dimensional scanner to quantify anecic earthworm burrows

Dye solution experiments for determining solute transport behaviour in degraded wetland soils of the Yellow River Delta

Contact Info

Product

Resources

About