Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China

Understanding the water movement in reconstructed soil and its efficacy on local vegetation is critical for the ecological reclamation of mine lands. This study employed field experiments and a numerical model to investigate the water movement in reconstructed soil and evaluate the effects of mining...

Full description

Bibliographic Details
Main Authors: Zizhao Zhang, Qianli Lv, Zezhou Guo, Xuebang Huang, Ruihua Hao
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/9/1240
id doaj-c7938ffbdbe149d2bc23676d7118012f
record_format Article
spelling doaj-c7938ffbdbe149d2bc23676d7118012f2021-04-29T23:03:00ZengMDPI AGWater2073-44412021-04-01131240124010.3390/w13091240Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, ChinaZizhao Zhang0Qianli Lv1Zezhou Guo2Xuebang Huang3Ruihua Hao4School of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, ChinaSchool of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, ChinaSchool of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, ChinaSchool of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, ChinaSchool of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, ChinaUnderstanding the water movement in reconstructed soil and its efficacy on local vegetation is critical for the ecological reclamation of mine lands. This study employed field experiments and a numerical model to investigate the water movement in reconstructed soil and evaluate the effects of mining waste rock on plant growth in an arid and cold region of Xinjiang. Water contents and matrix potentials were monitored over 1-year period. A numerical model was established based on the observed data to calculate soil water balance and irrigation demand. The results show that the soil water content at a shallow depth could be more vulnerable to the climate variability in uncompacted and compacted soil. The water content at the depth of 50 cm with 30 cm-thick covering soil was the lowest; meanwhile, the barrels with 50 cm- and 70 cm-thick covering soil without compaction had the highest water content. Moreover, the water content of the uncompacted soil could be lower than that of the counterpart attributed to the variation in soil porosity. To maintain the water content as an optimized value to grow a certain plant species in the long run, irrigation could be implemented according to the water balance over time in mine lands.https://www.mdpi.com/2073-4441/13/9/1240mine lands reclamationreconstructed soilwater movementplant growtharid and cold regions
collection DOAJ
language English
format Article
sources DOAJ
author Zizhao Zhang
Qianli Lv
Zezhou Guo
Xuebang Huang
Ruihua Hao
spellingShingle Zizhao Zhang
Qianli Lv
Zezhou Guo
Xuebang Huang
Ruihua Hao
Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China
Water
mine lands reclamation
reconstructed soil
water movement
plant growth
arid and cold regions
author_facet Zizhao Zhang
Qianli Lv
Zezhou Guo
Xuebang Huang
Ruihua Hao
author_sort Zizhao Zhang
title Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China
title_short Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China
title_full Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China
title_fullStr Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China
title_full_unstemmed Soil Water Movement of Mining Waste Rock and the Effect on Plant Growth in Arid, Cold Regions of Xinjiang, China
title_sort soil water movement of mining waste rock and the effect on plant growth in arid, cold regions of xinjiang, china
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-04-01
description Understanding the water movement in reconstructed soil and its efficacy on local vegetation is critical for the ecological reclamation of mine lands. This study employed field experiments and a numerical model to investigate the water movement in reconstructed soil and evaluate the effects of mining waste rock on plant growth in an arid and cold region of Xinjiang. Water contents and matrix potentials were monitored over 1-year period. A numerical model was established based on the observed data to calculate soil water balance and irrigation demand. The results show that the soil water content at a shallow depth could be more vulnerable to the climate variability in uncompacted and compacted soil. The water content at the depth of 50 cm with 30 cm-thick covering soil was the lowest; meanwhile, the barrels with 50 cm- and 70 cm-thick covering soil without compaction had the highest water content. Moreover, the water content of the uncompacted soil could be lower than that of the counterpart attributed to the variation in soil porosity. To maintain the water content as an optimized value to grow a certain plant species in the long run, irrigation could be implemented according to the water balance over time in mine lands.
topic mine lands reclamation
reconstructed soil
water movement
plant growth
arid and cold regions
url https://www.mdpi.com/2073-4441/13/9/1240
work_keys_str_mv AT zizhaozhang soilwatermovementofminingwasterockandtheeffectonplantgrowthinaridcoldregionsofxinjiangchina
AT qianlilv soilwatermovementofminingwasterockandtheeffectonplantgrowthinaridcoldregionsofxinjiangchina
AT zezhouguo soilwatermovementofminingwasterockandtheeffectonplantgrowthinaridcoldregionsofxinjiangchina
AT xuebanghuang soilwatermovementofminingwasterockandtheeffectonplantgrowthinaridcoldregionsofxinjiangchina
AT ruihuahao soilwatermovementofminingwasterockandtheeffectonplantgrowthinaridcoldregionsofxinjiangchina
_version_ 1721500244734115840