Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta

Water shortages due to low precipitation and seawater intrusion in the Lower China Yellow River Delta have occurred in recent years. Exploiting underground brackish water through well drilling is a potential alternative way to satisfy the demand for agricultural irrigation. However, how to successfu...

Full description

Bibliographic Details
Main Authors: Tianyu Wang, Zhenghe Xu, Guibin Pang
Format: Article
Language:English
Published: MDPI AG 2019-10-01
Series:Sustainability
Subjects:
Online Access:https://www.mdpi.com/2071-1050/11/20/5801
id doaj-6ba1a9b19fc44f80b176716ebc9de2fa
record_format Article
spelling doaj-6ba1a9b19fc44f80b176716ebc9de2fa2020-11-24T21:19:01ZengMDPI AGSustainability2071-10502019-10-011120580110.3390/su11205801su11205801Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River DeltaTianyu Wang0Zhenghe Xu1Guibin Pang2School of Water Conservancy and Environment, University of Jinan, Jinan 250022, ChinaSchool of Water Conservancy and Environment, University of Jinan, Jinan 250022, ChinaSchool of Water Conservancy and Environment, University of Jinan, Jinan 250022, ChinaWater shortages due to low precipitation and seawater intrusion in the Lower China Yellow River Delta have occurred in recent years. Exploiting underground brackish water through well drilling is a potential alternative way to satisfy the demand for agricultural irrigation. However, how to successfully use brackish water for irrigation has become a new problem to solve. A two-year field experiment was conducted in this typical saline-alkaline region to investigate the effects of irrigating with brackish water on the soil water-salt dynamics, and the physiological response of winter wheat to drought-salt stress. The experiment was laid out in a randomized block design with three replications according to the quantity (160 mm and 240 mm) and quality (fresh water and brackish water with a salt concentration of 3 g L<sup>&#8722;1</sup>) of irrigation water: T1 was 240 mm of fresh water, T2 was 160 mm of fresh water, T3 was 80 mm of fresh water and 160 mm of brackish water, and T4 was 80 mm of fresh water and 80 mm of brackish water. The results showed that the soil moisture of T3 was almost the same as T1 after the harvest of winter wheat each year, therefore, irrigating with brackish water can maintain soil moisture while saving fresh water resources. After two years, the soil salinity of each treatment increased by 0.307, 0.406, 0.383, and 0.889 g kg<sup>&#8722;1</sup>, respectively. During the jointing-flowering stage, salt stress has a significant inhibitory effect on photosynthesis; T3 and T4 were lower than T1 and T2 in terms of plant height and dry weight. During the filling stage, because the effect of drought stress is more serious than that of salt stress, the photosynthesis of T3 was greater than that of T2 and T4. For both years, the yield of crops followed the rank order T1 &gt; T3 &gt; T2 &gt; T4. Compared with irrigating with fresh water in T1, T3 changed the second and third irrigation into brackish water, however we did not find that soil salinity increased significantly, and this treatment was able to ensure crop growth during the filling stage. Therefore, the combination of fresh water (80 mm), then brackish water (80 mm), then brackish water (80 mm) is a feasible irrigation strategy in China&#8217;s Yellow River Delta for winter wheat.https://www.mdpi.com/2071-1050/11/20/5801irrigation strategieswater quality and quantitysoil salt accumulationagronomic traitsphotosynthesis
collection DOAJ
language English
format Article
sources DOAJ
author Tianyu Wang
Zhenghe Xu
Guibin Pang
spellingShingle Tianyu Wang
Zhenghe Xu
Guibin Pang
Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta
Sustainability
irrigation strategies
water quality and quantity
soil salt accumulation
agronomic traits
photosynthesis
author_facet Tianyu Wang
Zhenghe Xu
Guibin Pang
author_sort Tianyu Wang
title Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta
title_short Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta
title_full Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta
title_fullStr Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta
title_full_unstemmed Effects of Irrigating with Brackish Water on Soil Moisture, Soil Salinity, and the Agronomic Response of Winter Wheat in the Yellow River Delta
title_sort effects of irrigating with brackish water on soil moisture, soil salinity, and the agronomic response of winter wheat in the yellow river delta
publisher MDPI AG
series Sustainability
issn 2071-1050
publishDate 2019-10-01
description Water shortages due to low precipitation and seawater intrusion in the Lower China Yellow River Delta have occurred in recent years. Exploiting underground brackish water through well drilling is a potential alternative way to satisfy the demand for agricultural irrigation. However, how to successfully use brackish water for irrigation has become a new problem to solve. A two-year field experiment was conducted in this typical saline-alkaline region to investigate the effects of irrigating with brackish water on the soil water-salt dynamics, and the physiological response of winter wheat to drought-salt stress. The experiment was laid out in a randomized block design with three replications according to the quantity (160 mm and 240 mm) and quality (fresh water and brackish water with a salt concentration of 3 g L<sup>&#8722;1</sup>) of irrigation water: T1 was 240 mm of fresh water, T2 was 160 mm of fresh water, T3 was 80 mm of fresh water and 160 mm of brackish water, and T4 was 80 mm of fresh water and 80 mm of brackish water. The results showed that the soil moisture of T3 was almost the same as T1 after the harvest of winter wheat each year, therefore, irrigating with brackish water can maintain soil moisture while saving fresh water resources. After two years, the soil salinity of each treatment increased by 0.307, 0.406, 0.383, and 0.889 g kg<sup>&#8722;1</sup>, respectively. During the jointing-flowering stage, salt stress has a significant inhibitory effect on photosynthesis; T3 and T4 were lower than T1 and T2 in terms of plant height and dry weight. During the filling stage, because the effect of drought stress is more serious than that of salt stress, the photosynthesis of T3 was greater than that of T2 and T4. For both years, the yield of crops followed the rank order T1 &gt; T3 &gt; T2 &gt; T4. Compared with irrigating with fresh water in T1, T3 changed the second and third irrigation into brackish water, however we did not find that soil salinity increased significantly, and this treatment was able to ensure crop growth during the filling stage. Therefore, the combination of fresh water (80 mm), then brackish water (80 mm), then brackish water (80 mm) is a feasible irrigation strategy in China&#8217;s Yellow River Delta for winter wheat.
topic irrigation strategies
water quality and quantity
soil salt accumulation
agronomic traits
photosynthesis
url https://www.mdpi.com/2071-1050/11/20/5801
work_keys_str_mv AT tianyuwang effectsofirrigatingwithbrackishwateronsoilmoisturesoilsalinityandtheagronomicresponseofwinterwheatintheyellowriverdelta
AT zhenghexu effectsofirrigatingwithbrackishwateronsoilmoisturesoilsalinityandtheagronomicresponseofwinterwheatintheyellowriverdelta
AT guibinpang effectsofirrigatingwithbrackishwateronsoilmoisturesoilsalinityandtheagronomicresponseofwinterwheatintheyellowriverdelta
_version_ 1726007261265920000