Soil macroporosity and water flow in the root zone of oases in hyper-arid regions

被引:6
|
作者
Zhang, Yongyong [1 ,2 ]
Jia, Angyuan [3 ]
Zhao, Wenzhi [1 ,2 ]
Kang, Jianjun [1 ,2 ]
Wang, Chuan [1 ,2 ]
Kang, Wenrong [1 ,2 ]
Tian, Zihan [1 ,2 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Ecohydrol Inland River Basin, Line Inland River Basin Res Stn, Lanzhou 730000, Peoples R China
[2] Univ Chinese Acad Sci, Beijing, Peoples R China
[3] Chinese Acad Agr Sci, Inst Agr Resources & Reg Planning, Natl Engn Lab Improving Qual Arable Land, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
dye tracer; preferential flow; soil structure; water infiltration; X-ray tomography; DESERT-OASIS ECOTONE; PREFERENTIAL FLOW; IMAGE-ANALYSIS; INFILTRATION; INFILTRABILITY; TRANSPORT; PATTERNS; TREES;
D O I
10.1111/ejss.13235
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The characteristics of soil macropores and water infiltration are closely connected to the growth of plant roots and their root zone environment. However, it is unclear how the root zone environment of oasis farmlands regulates the development of soil macropores and water flow in hyper-arid regions. The objective of this study was to investigate soil macropores and their effect on water flow under irrigated oasis farmlands using a combination of X-ray computed tomography (CT) and dye tracer. It was hypothesized that the integration of CT and dye tracer could clearly reveal preferential flow through biopores and large pores of oasis soils. A helical medical CT scanner was used to quantify more information about soil macropores in the root zone, along with an in situ single-ring dye infiltration experiment to reveal water flow in three different oasis farmlands (piedmont oasis farmland, marginal oasis farmland, and old oasis farmland). Soil macroporosity was 0.44% under crop rows, while soil macroporosity in the interrows was only 0.30% across the oasis farmlands. Biopores contributed 73% of the volume of the total macropores under crop rows. The stable infiltration rate in the interrows was 0.3 mm min(-1), which was significantly (p < 0.05) less than that under crop rows (0.7 mm min(-1)). Water flow under crop rows were mainly transported in biopores and large pores. The contribution of macropores to preferential flow under crop rows was 4.8 times larger than interrows. The integration of CT and dye tracer was a more holistic technique, which adequately revealed that oases had preferential flow affected by biopores and large pores, resulting in higher solute and contaminant transport. Key Points Soil macropores and preferential flow affected by crop roots were investigated in hyper-arid regions. The integration of CT and dye tracer adequately identified preferential flowpaths of oasis soils. Biopores were larger under crop rows than interrows. Preferential flow transported in biopores and large soil pores under crop rows.
引用
收藏
页数:14
相关论文
共 50 条
  • [1] Cryospheric processes in Quaternary and Cretaceous hyper-arid plateau desert oases
    Wu, Chihua
    Rodriguez-Lopez, Juan Pedro
    [J]. SEDIMENTOLOGY, 2021, 68 (02) : 755 - 770
  • [2] Multiple sources characteristics of root water uptake of crop under oasis farmlands in hyper-arid regions
    Zhang, Yongyong
    Wu, Shaoxiong
    Kang, Wenrong
    Tian, Zihan
    [J]. AGRICULTURAL WATER MANAGEMENT, 2022, 271
  • [3] Responses of phreatophyte transpiration to falling water table in hyper-arid and arid regions, Northwest China
    Yin, Li-he
    Xu, Dan-dan
    Jia, Wu-hui
    Zhang, Xin-xin
    Zhang, Jun
    [J]. CHINA GEOLOGY, 2021, 4 (03) : 410 - 420
  • [4] Responses of phreatophyte transpiration to falling water table in hyper-arid and arid regions, Northwest China
    Li-he Yin
    Dan-dan Xu
    Wu-hui Jia
    Xin-xin Zhang
    Jun Zhang
    [J]. China Geology, 2021, 4 (03) : 410 - 420
  • [5] Modelling Soil Moisture in Hyper-Arid Conditions
    Yaping Shao
    Klaus Fraedrich
    Masahide Ishizuka
    [J]. Boundary-Layer Meteorology, 2021, 179 : 169 - 186
  • [6] Modelling Soil Moisture in Hyper-Arid Conditions
    Shao, Yaping
    Fraedrich, Klaus
    Ishizuka, Masahide
    [J]. BOUNDARY-LAYER METEOROLOGY, 2021, 179 (02) : 169 - 186
  • [7] The autecological characteristics of Desmostachya bipinnata in hyper-arid regions
    Fakhireh, Akbar
    Ajorlo, Majid
    Shahryari, Alireza
    Mansouri, Shahram
    Nouri, Soheila
    Pahlavanravi, Ahmad
    [J]. TURKISH JOURNAL OF BOTANY, 2012, 36 (06) : 690 - 696
  • [8] Satellite-Based Monitoring of Growing Agricultural Water Consumption in Hyper-Arid Regions
    Ebrahimivand, Ashkan
    Hooshyaripor, Farhad
    Rezaei-Gharehaghaj, Salar
    Razi, Sahand
    Salamttalab, Mohammad Milad
    Kolahi, Mahdi
    Noori, Roohollah
    [J]. WATER, 2023, 15 (22)
  • [9] CHANGING RAINFALL, SEASONALITY AND EROSIVITY IN THE HYPER-ARID ZONE OF SUDAN
    Elagib, N. A.
    [J]. LAND DEGRADATION & DEVELOPMENT, 2011, 22 (06) : 505 - 512
  • [10] Water-Table Detection in a Hyper-Arid Region
    Lai, Zhi-Hong
    Kiang, Jean-Fu
    [J]. 2019 USNC-URSI RADIO SCIENCE MEETING (JOINT WITH AP-S SYMPOSIUM), 2019, : 107 - 108