Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China

Textural layering of soil plays an important role in distributing and regulating resources for plants in many semiarid and arid landscapes. However, the spatial patterns of textural layering and the potential effects on soil hydrology and water regimes are poorly understood, especially in arid sandy...

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Main Authors: Chengpeng Sun, Wenzhi Zhao, Hu Liu, Yongyong Zhang, Hong Zhou
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-02-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.627500/full
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author Chengpeng Sun
Chengpeng Sun
Chengpeng Sun
Wenzhi Zhao
Wenzhi Zhao
Hu Liu
Hu Liu
Yongyong Zhang
Yongyong Zhang
Hong Zhou
author_facet Chengpeng Sun
Chengpeng Sun
Chengpeng Sun
Wenzhi Zhao
Wenzhi Zhao
Hu Liu
Hu Liu
Yongyong Zhang
Yongyong Zhang
Hong Zhou
author_sort Chengpeng Sun
collection DOAJ
description Textural layering of soil plays an important role in distributing and regulating resources for plants in many semiarid and arid landscapes. However, the spatial patterns of textural layering and the potential effects on soil hydrology and water regimes are poorly understood, especially in arid sandy soil environments like the desert-oasis ecotones in northwestern China. This work aims to determine the distribution of textural layered soils, analyze the effects of different soil-textural configurations on water regimes, and evaluate which factors affect soil water infiltration and retention characteristics in such a desert-oasis ecotone. We measured soil water content and mineral composition in 87 soil profiles distributed along three transects in the study area. Constant-head infiltration experiments were conducted at 9 of the soil profiles with different texture configurations. The results showed that textural layered soils were patchily but extensively distributed throughout the study area (with a combined surface area percentage of about 84%). Soil water content in the profiles ranged from 0.002 to 0.27 g/cm3 during the investigation period, and significantly and positively correlated with the thickness of a medium-textured (silt or silt loam) layer (p < 0.001). The occurrence of a medium-textured layer increased field capacity and wilting point and decreased available water-holding capacity in soil profiles. Burial depth of the medium-textured layer had no clear effects on water retention properties, but the layer thickness tended to. In textural layered soils, smaller water infiltration rate and cumulative infiltration, and shallower depths of wetting fronts were detected, compared with homogeneous sand profiles. The thickness and burial depth of medium-textured layers had obvious effects on infiltration, but the magnitude of the effects depended on soil texture configuration. The revealed patterns of soil textural layering and the potential effects on water regimes may provide new insight into the sustainable management of rainfed vegetation in the desert-oasis ecotones of arid northwestern China and other regions with similar environments around the world.
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spelling doaj.art-7bdd5ed246b44e52a1a3584a44229e0c2022-12-21T22:47:44ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-02-01910.3389/feart.2021.627500627500Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern ChinaChengpeng Sun0Chengpeng Sun1Chengpeng Sun2Wenzhi Zhao3Wenzhi Zhao4Hu Liu5Hu Liu6Yongyong Zhang7Yongyong Zhang8Hong Zhou9Key Laboratory of Ecohydrology and River Basin Science, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaLinze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou, ChinaCollege of Resources and Environment, University of Chinese Academy of Sciences, Beijing, ChinaKey Laboratory of Ecohydrology and River Basin Science, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaLinze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou, ChinaKey Laboratory of Ecohydrology and River Basin Science, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaLinze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou, ChinaKey Laboratory of Ecohydrology and River Basin Science, Northwest Institute of Eco-environment and Resources, Chinese Academy of Sciences, Lanzhou, ChinaLinze Inland River Basin Research Station, Chinese Ecosystem Research Network, Lanzhou, ChinaTourism College, Northwest Normal University, Lanzhou, ChinaTextural layering of soil plays an important role in distributing and regulating resources for plants in many semiarid and arid landscapes. However, the spatial patterns of textural layering and the potential effects on soil hydrology and water regimes are poorly understood, especially in arid sandy soil environments like the desert-oasis ecotones in northwestern China. This work aims to determine the distribution of textural layered soils, analyze the effects of different soil-textural configurations on water regimes, and evaluate which factors affect soil water infiltration and retention characteristics in such a desert-oasis ecotone. We measured soil water content and mineral composition in 87 soil profiles distributed along three transects in the study area. Constant-head infiltration experiments were conducted at 9 of the soil profiles with different texture configurations. The results showed that textural layered soils were patchily but extensively distributed throughout the study area (with a combined surface area percentage of about 84%). Soil water content in the profiles ranged from 0.002 to 0.27 g/cm3 during the investigation period, and significantly and positively correlated with the thickness of a medium-textured (silt or silt loam) layer (p < 0.001). The occurrence of a medium-textured layer increased field capacity and wilting point and decreased available water-holding capacity in soil profiles. Burial depth of the medium-textured layer had no clear effects on water retention properties, but the layer thickness tended to. In textural layered soils, smaller water infiltration rate and cumulative infiltration, and shallower depths of wetting fronts were detected, compared with homogeneous sand profiles. The thickness and burial depth of medium-textured layers had obvious effects on infiltration, but the magnitude of the effects depended on soil texture configuration. The revealed patterns of soil textural layering and the potential effects on water regimes may provide new insight into the sustainable management of rainfed vegetation in the desert-oasis ecotones of arid northwestern China and other regions with similar environments around the world.https://www.frontiersin.org/articles/10.3389/feart.2021.627500/fullTextural layeringSoil hydrologyWater retentionWater infiltrationWater regimes
spellingShingle Chengpeng Sun
Chengpeng Sun
Chengpeng Sun
Wenzhi Zhao
Wenzhi Zhao
Hu Liu
Hu Liu
Yongyong Zhang
Yongyong Zhang
Hong Zhou
Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China
Frontiers in Earth Science
Textural layering
Soil hydrology
Water retention
Water infiltration
Water regimes
title Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China
title_full Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China
title_fullStr Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China
title_full_unstemmed Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China
title_short Effects of Textural Layering on Water Regimes in Sandy Soils in a Desert-Oasis Ecotone, Northwestern China
title_sort effects of textural layering on water regimes in sandy soils in a desert oasis ecotone northwestern china
topic Textural layering
Soil hydrology
Water retention
Water infiltration
Water regimes
url https://www.frontiersin.org/articles/10.3389/feart.2021.627500/full
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