The third principle of water flow in soils

H. Lin; L. Guo; L. Feng

The third principle of water flow in soils

H. Lin, L. Guo, L. Feng

Research output: Contribution to conference › Paper › peer-review

Abstract

Water flow in soils is fundamental to subsurface hydrology, biogeochemical cycling, contaminant transport, and ecosystem services. It has taken three centuries for three principles of water flow in soils to be identified. The first came to light in the 19th century, known as the Darcy's law. The second was formally proposed by L.A. Richards in the 20th century. The third principle is emerging in the 21^st century, where a combined macroscopic and microscopic consideration portrays complex preferential flow networks embedded in heterogeneous soils. This 3r^d principle is presented and illustrated in this paper.

Original language	English (US)
Pages	60-64
Number of pages	5
State	Published - Jan 1 2019
Event	20th Annual Conference of the International Association for Mathematical Geosciences, IAMG 2019 - State College, United States Duration: Aug 10 2019 → Aug 16 2019

Conference

Conference	20th Annual Conference of the International Association for Mathematical Geosciences, IAMG 2019
Country/Territory	United States
City	State College
Period	8/10/19 → 8/16/19

All Science Journal Classification (ASJC) codes

Earth and Planetary Sciences(all)
Mathematics (miscellaneous)

Cite this

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abstract = "Water flow in soils is fundamental to subsurface hydrology, biogeochemical cycling, contaminant transport, and ecosystem services. It has taken three centuries for three principles of water flow in soils to be identified. The first came to light in the 19th century, known as the Darcy's law. The second was formally proposed by L.A. Richards in the 20th century. The third principle is emerging in the 21st century, where a combined macroscopic and microscopic consideration portrays complex preferential flow networks embedded in heterogeneous soils. This 3rd principle is presented and illustrated in this paper.",

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AU - Lin, H.

AU - Guo, L.

AU - Feng, L.

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N2 - Water flow in soils is fundamental to subsurface hydrology, biogeochemical cycling, contaminant transport, and ecosystem services. It has taken three centuries for three principles of water flow in soils to be identified. The first came to light in the 19th century, known as the Darcy's law. The second was formally proposed by L.A. Richards in the 20th century. The third principle is emerging in the 21st century, where a combined macroscopic and microscopic consideration portrays complex preferential flow networks embedded in heterogeneous soils. This 3rd principle is presented and illustrated in this paper.

AB - Water flow in soils is fundamental to subsurface hydrology, biogeochemical cycling, contaminant transport, and ecosystem services. It has taken three centuries for three principles of water flow in soils to be identified. The first came to light in the 19th century, known as the Darcy's law. The second was formally proposed by L.A. Richards in the 20th century. The third principle is emerging in the 21st century, where a combined macroscopic and microscopic consideration portrays complex preferential flow networks embedded in heterogeneous soils. This 3rd principle is presented and illustrated in this paper.

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M3 - Paper

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T2 - 20th Annual Conference of the International Association for Mathematical Geosciences, IAMG 2019

Y2 - 10 August 2019 through 16 August 2019

ER -

The third principle of water flow in soils

Abstract

Conference

All Science Journal Classification (ASJC) codes

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