干旱区生态环境知识资源中心(Arid): Interaction Between Brackish Water Intermittent Infiltration and Cultivated Soil Environment: A Case Study From Arid Piedmont Plain of Northwest China

Arid

DOI	10.3389/feart.2022.894033
	Interaction Between Brackish Water Intermittent Infiltration and Cultivated Soil Environment: A Case Study From Arid Piedmont Plain of Northwest China
	Leilei, Guo; Zaimin, Wang
通讯作者	Zaimin, W
来源期刊	FRONTIERS IN EARTH SCIENCE
EISSN	2296-6463
出版年	2022
卷号	10
英文摘要	Brackish groundwater was widely used in arid areas which may cause soil salinization and groundwater environmental declines. To ensure the sustainable development of agriculture in arid areas, brackish water intermittent infiltration experiments were conducted in Southern Xinjiang, Northwest China between June to September 2018, and Hydrus-2D numerical simulation was used to analyze the underground pipe drainage systems. The field experiments were carried out during cotton growth stages after the first freshwater flood infiltration and salt washing. Two control experiments were, respectively, designed as freshwater (0.68 g/L) and brackish water (1.66 g/L) with water amount of 1.0 Q = 572 mm. Other eight groups (1.05-1.40 Q) were compared to analyze the effect of soil salt leaching by increasing the brackish water amount. The results showed that the soil moisture content was almost less than the field capacity of 0.203 at depth of 0-60 cm before each infiltration due to roots water uptake, and the soil water holding capacity rate was lower than 0.2 after 5 days under 1.20-1.40 Q brackish water treatments. Variation of EC1:5 at depth of 0-30 cm was less than 0.5 dS/m. Salt mainly accumulated at the depth of 40-60 cm whether the water amount was excessive or insufficient even under the fresh water infiltration. The optimal brackish water amount was 1.15 Q = 657.8 mm, and the soil total salinity was less than 0.55 dS/m (EC1:5) and reached mild salinization degree. Numerical simulations were used based on the 2018 field experimental results and extended by another 10 years. The soil salt accumulated to 1.10-2.99 dS/m (EC1:5) at the depth of 40-60 cm during 0-30 days. The no salinization area expanded to depth of 40-45 cm after 120 days and reduced during non-infiltration period due to evaporation effect. The soil salt was gradually leached and less than 0.55 dS/m (EC1:5) after 10 years. The optimized leaching-drainage system could not only provide a low salinity soil condition for cotton growth and realize sustainable cultivation but also greatly protect the soil and groundwater environment.
英文关键词	brackish water intermittent infiltration arid area salt accumulation numerical simulations leaching-drainage system Hydrus-2D
类型	Article
语种	英语
开放获取类型	gold
收录类别	SCI-E
WOS记录号	WOS:000812086400001
WOS关键词	MULCHED DRIP IRRIGATION ; SPATIAL-DISTRIBUTION ; COTTON FIELD ; SALINE WATER ; SALT ; MOVEMENT ; CONDUCTIVITY ; SIMULATIONS ; TRANSPORT ; MOISTURE
WOS类目	Geosciences, Multidisciplinary
WOS研究方向	Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/392674
推荐引用方式 GB/T 7714	Leilei, Guo,Zaimin, Wang. Interaction Between Brackish Water Intermittent Infiltration and Cultivated Soil Environment: A Case Study From Arid Piedmont Plain of Northwest China[J],2022,10.
APA	Leilei, Guo,&Zaimin, Wang.(2022).Interaction Between Brackish Water Intermittent Infiltration and Cultivated Soil Environment: A Case Study From Arid Piedmont Plain of Northwest China.FRONTIERS IN EARTH SCIENCE,10.
MLA	Leilei, Guo,et al."Interaction Between Brackish Water Intermittent Infiltration and Cultivated Soil Environment: A Case Study From Arid Piedmont Plain of Northwest China".FRONTIERS IN EARTH SCIENCE 10(2022).