Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.

Groundwater is the main water resource for plant growth and development in the saline soil of the Yellow River Delta in China. To investigate the variabilities and distributions of soil water and salt contents at various groundwater level (GL), soil columns with planting Tamarix chinensis Lour were...

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Main Authors: Jiangbao Xia, Ximei Zhao, Yinping Chen, Ying Fang, Ziguo Zhao
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2016-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC4701359?pdf=render
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spelling doaj-d90a4f3e42454ba18955f0dadf5232f92020-11-25T02:05:57ZengPublic Library of Science (PLoS)PLoS ONE1932-62032016-01-01111e014582810.1371/journal.pone.0145828Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.Jiangbao XiaXimei ZhaoYinping ChenYing FangZiguo ZhaoGroundwater is the main water resource for plant growth and development in the saline soil of the Yellow River Delta in China. To investigate the variabilities and distributions of soil water and salt contents at various groundwater level (GL), soil columns with planting Tamarix chinensis Lour were established at six different GL. The results demonstrated the following: With increasing GL, the relative soil water content (RWC) declined significantly, whereas the salt content (SC) and absolute soil solution concentration (CS) decreased after the initial increase in the different soil profiles. A GL of 1.2 m was the turning point for variations in the soil water and salt contents, and it represented the highest GL that could maintain the soil surface moist within the soil columns. Both the SC and CS reached the maximum levels in these different soil profiles at a GL of 1.2 m. With the raise of soil depth, the RWC increased significantly, whereas the SC increased after an initial decrease. The mean SC values reached 0.96% in the top soil layer; however, the rates at which the CS and RWC decreased with the GL were significantly reduced. The RWC and SC presented the greatest variations at the medium (0.9-1.2 m) and shallow water levels (0.6 m) respectively, whereas the CS presented the greatest variation at the deep water level (1.5-1.8 m).The RWC, SC and CS in the soil columns were all closely related to the GL. However, the correlations among the parameters varied greatly within different soil profiles, and the most accurate predictions of the GL were derived from the RWC in the shallow soil layer or the SC in the top soil layer. A GL at 1.5-1.8 m was moderate for planting T. chinensis seedlings under saline groundwater conditions.http://europepmc.org/articles/PMC4701359?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Jiangbao Xia
Ximei Zhao
Yinping Chen
Ying Fang
Ziguo Zhao
spellingShingle Jiangbao Xia
Ximei Zhao
Yinping Chen
Ying Fang
Ziguo Zhao
Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.
PLoS ONE
author_facet Jiangbao Xia
Ximei Zhao
Yinping Chen
Ying Fang
Ziguo Zhao
author_sort Jiangbao Xia
title Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.
title_short Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.
title_full Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.
title_fullStr Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.
title_full_unstemmed Responses of Water and Salt Parameters to Groundwater Levels for Soil Columns Planted with Tamarix chinensis.
title_sort responses of water and salt parameters to groundwater levels for soil columns planted with tamarix chinensis.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2016-01-01
description Groundwater is the main water resource for plant growth and development in the saline soil of the Yellow River Delta in China. To investigate the variabilities and distributions of soil water and salt contents at various groundwater level (GL), soil columns with planting Tamarix chinensis Lour were established at six different GL. The results demonstrated the following: With increasing GL, the relative soil water content (RWC) declined significantly, whereas the salt content (SC) and absolute soil solution concentration (CS) decreased after the initial increase in the different soil profiles. A GL of 1.2 m was the turning point for variations in the soil water and salt contents, and it represented the highest GL that could maintain the soil surface moist within the soil columns. Both the SC and CS reached the maximum levels in these different soil profiles at a GL of 1.2 m. With the raise of soil depth, the RWC increased significantly, whereas the SC increased after an initial decrease. The mean SC values reached 0.96% in the top soil layer; however, the rates at which the CS and RWC decreased with the GL were significantly reduced. The RWC and SC presented the greatest variations at the medium (0.9-1.2 m) and shallow water levels (0.6 m) respectively, whereas the CS presented the greatest variation at the deep water level (1.5-1.8 m).The RWC, SC and CS in the soil columns were all closely related to the GL. However, the correlations among the parameters varied greatly within different soil profiles, and the most accurate predictions of the GL were derived from the RWC in the shallow soil layer or the SC in the top soil layer. A GL at 1.5-1.8 m was moderate for planting T. chinensis seedlings under saline groundwater conditions.
url http://europepmc.org/articles/PMC4701359?pdf=render
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AT yinpingchen responsesofwaterandsaltparameterstogroundwaterlevelsforsoilcolumnsplantedwithtamarixchinensis
AT yingfang responsesofwaterandsaltparameterstogroundwaterlevelsforsoilcolumnsplantedwithtamarixchinensis
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