Evaluation of seasonal patterns of hydraulic redistribution in a humid subtropical area, East China

Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is defined as water distributed (typically at night) from moist soil to drier soil via plant roots, which plays an important role in soil moistu...

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Published inHydrological processes Vol. 34; no. 4; pp. 1052 - 1062
Main Authors Sun, Long, Yang, Lei, Chen, Liding, Yen, Haw, Zhao, Fangkai, Li, Shoujuan
Format Journal Article
LanguageEnglish
Published Chichester Wiley Subscription Services, Inc 15.02.2020
Subjects
antecedent soil moisture
Camphor
China
Environmental monitoring
Growing season
Humid areas
humid zones
Hydrologic processes
Hydrologic studies
Hydrology
Moisture content
monitoring
normalized hydraulic redistribution
peaches
Plant roots
Replenishment
roots
seasonal variation
Seasonal variations
Seasons
shallow soil
Soil
Soil investigations
Soil moisture
Soil moisture content
soil moisture dynamics
Soil water
soil water content
soil water use
Soils
summer
temporal variation
Temporal variations
Water content
Water depth
water replenishment
Water use
Zhangxi watershed
China
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Abstract Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is defined as water distributed (typically at night) from moist soil to drier soil via plant roots, which plays an important role in soil moisture replenishment. Knowledge on seasonal patterns of HR and on the relationship between HR and soil water use is not fully understood. We investigated temporal variations in HR and total daily water use (Δθ) at stands of camphor and peach by monitoring soil moisture content in a humid region in eastern China. HR at the three locations reached its maximum values in summer (0.68 mm d−1 to 1.15 mm d−1) at depths of 15 cm and 35 cm. Redistributed water replenished 41% of water depleted in the soil at a 5–45‐cm depth. Interestingly, normalized HR (i.e., HR/Δθ) showed a constant pattern during the growing season implying it is independent of seasonal climate alterations. This also indicated that HR had a stable effect on the replenishment of daily water use. Positive linear relationships between HR and Δθ were found at three measuring locations (camphor: R2 = .35, p < .01; peach1: R2 = .57, p < .01; peach2: R2 = .63, p < .01), suggesting a relatively stable inherent linkage between HR and Δθ. This study suggested that hydrological processes involving soil moisture status or antecedent soil moisture, needs to take the HR effect into account across timescales from intraday to seasonal. Positive linear relationship was found between hydraulic redistribution (HR) and total daily water use (Δθ) at the three monitoring locations. Normalized HR (i.e., HR/Δθ) showed a constant pattern during the growing season, implying it is independent of seasonal climate alterations. Hydrological processes involving soil moisture status or antecedent soil moisture needs take the HR effect into account across timescales from intra‐day to seasonal.
AbstractList Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is defined as water distributed (typically at night) from moist soil to drier soil via plant roots, which plays an important role in soil moisture replenishment. Knowledge on seasonal patterns of HR and on the relationship between HR and soil water use is not fully understood. We investigated temporal variations in HR and total daily water use (Δθ) at stands of camphor and peach by monitoring soil moisture content in a humid region in eastern China. HR at the three locations reached its maximum values in summer (0.68 mm d−1 to 1.15 mm d−1) at depths of 15 cm and 35 cm. Redistributed water replenished 41% of water depleted in the soil at a 5–45‐cm depth. Interestingly, normalized HR (i.e., HR/Δθ) showed a constant pattern during the growing season implying it is independent of seasonal climate alterations. This also indicated that HR had a stable effect on the replenishment of daily water use. Positive linear relationships between HR and Δθ were found at three measuring locations (camphor: R2 = .35, p < .01; peach1: R2 = .57, p < .01; peach2: R2 = .63, p < .01), suggesting a relatively stable inherent linkage between HR and Δθ. This study suggested that hydrological processes involving soil moisture status or antecedent soil moisture, needs to take the HR effect into account across timescales from intraday to seasonal.
Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is defined as water distributed (typically at night) from moist soil to drier soil via plant roots, which plays an important role in soil moisture replenishment. Knowledge on seasonal patterns of HR and on the relationship between HR and soil water use is not fully understood. We investigated temporal variations in HR and total daily water use (Δ θ ) at stands of camphor and peach by monitoring soil moisture content in a humid region in eastern China. HR at the three locations reached its maximum values in summer (0.68 mm d −1 to 1.15 mm d −1 ) at depths of 15 cm and 35 cm. Redistributed water replenished 41% of water depleted in the soil at a 5–45‐cm depth. Interestingly, normalized HR (i.e., HR/Δ θ ) showed a constant pattern during the growing season implying it is independent of seasonal climate alterations. This also indicated that HR had a stable effect on the replenishment of daily water use. Positive linear relationships between HR and Δ θ were found at three measuring locations (camphor: R 2 = .35, p < .01; peach1: R 2 = .57, p < .01; peach2: R 2 = .63, p < .01), suggesting a relatively stable inherent linkage between HR and Δ θ. This study suggested that hydrological processes involving soil moisture status or antecedent soil moisture, needs to take the HR effect into account across timescales from intraday to seasonal.
Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is defined as water distributed (typically at night) from moist soil to drier soil via plant roots, which plays an important role in soil moisture replenishment. Knowledge on seasonal patterns of HR and on the relationship between HR and soil water use is not fully understood. We investigated temporal variations in HR and total daily water use (Δθ) at stands of camphor and peach by monitoring soil moisture content in a humid region in eastern China. HR at the three locations reached its maximum values in summer (0.68 mm d−1 to 1.15 mm d−1) at depths of 15 cm and 35 cm. Redistributed water replenished 41% of water depleted in the soil at a 5–45‐cm depth. Interestingly, normalized HR (i.e., HR/Δθ) showed a constant pattern during the growing season implying it is independent of seasonal climate alterations. This also indicated that HR had a stable effect on the replenishment of daily water use. Positive linear relationships between HR and Δθ were found at three measuring locations (camphor: R2 = .35, p < .01; peach1: R2 = .57, p < .01; peach2: R2 = .63, p < .01), suggesting a relatively stable inherent linkage between HR and Δθ. This study suggested that hydrological processes involving soil moisture status or antecedent soil moisture, needs to take the HR effect into account across timescales from intraday to seasonal. Positive linear relationship was found between hydraulic redistribution (HR) and total daily water use (Δθ) at the three monitoring locations. Normalized HR (i.e., HR/Δθ) showed a constant pattern during the growing season, implying it is independent of seasonal climate alterations. Hydrological processes involving soil moisture status or antecedent soil moisture needs take the HR effect into account across timescales from intra‐day to seasonal.
Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is defined as water distributed (typically at night) from moist soil to drier soil via plant roots, which plays an important role in soil moisture replenishment. Knowledge on seasonal patterns of HR and on the relationship between HR and soil water use is not fully understood. We investigated temporal variations in HR and total daily water use (Δθ) at stands of camphor and peach by monitoring soil moisture content in a humid region in eastern China. HR at the three locations reached its maximum values in summer (0.68 mm d⁻¹ to 1.15 mm d⁻¹) at depths of 15 cm and 35 cm. Redistributed water replenished 41% of water depleted in the soil at a 5–45‐cm depth. Interestingly, normalized HR (i.e., HR/Δθ) showed a constant pattern during the growing season implying it is independent of seasonal climate alterations. This also indicated that HR had a stable effect on the replenishment of daily water use. Positive linear relationships between HR and Δθ were found at three measuring locations (camphor: R² = .35, p < .01; peach1: R² = .57, p < .01; peach2: R² = .63, p < .01), suggesting a relatively stable inherent linkage between HR and Δθ. This study suggested that hydrological processes involving soil moisture status or antecedent soil moisture, needs to take the HR effect into account across timescales from intraday to seasonal.
Author Li, Shoujuan
Yang, Lei
Zhao, Fangkai
Yen, Haw
Chen, Liding
Sun, Long
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  orcidid: 0000-0002-2811-9009
  surname: Sun
  fullname: Sun, Long
  organization: Chinese Academy of Sciences
– sequence: 2
  givenname: Lei
  surname: Yang
  fullname: Yang, Lei
  email: leiyang@rcees.ac.cn
  organization: Chinese Academy of Sciences
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  givenname: Liding
  surname: Chen
  fullname: Chen, Liding
  organization: University of Chinese Academy of Sciences
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  givenname: Haw
  surname: Yen
  fullname: Yen, Haw
  organization: Texas A&M University
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  givenname: Fangkai
  surname: Zhao
  fullname: Zhao, Fangkai
  organization: University of Chinese Academy of Sciences
– sequence: 6
  givenname: Shoujuan
  surname: Li
  fullname: Li, Shoujuan
  organization: University of Chinese Academy of Sciences
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Snippet Antecedent soil moisture or soil moisture status has a great impact on hydrological processes. Hydraulic redistribution (HR), a widely observed phenomenon, is...
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SubjectTerms antecedent soil moisture
Camphor
China
Environmental monitoring
Growing season
Humid areas
humid zones
Hydrologic processes
Hydrologic studies
Hydrology
Moisture content
monitoring
normalized hydraulic redistribution
peaches
Plant roots
Replenishment
roots
seasonal variation
Seasonal variations
Seasons
shallow soil
Soil
Soil investigations
Soil moisture
Soil moisture content
soil moisture dynamics
Soil water
soil water content
soil water use
Soils
summer
temporal variation
Temporal variations
Water content
Water depth
water replenishment
Water use
Zhangxi watershed
Title Evaluation of seasonal patterns of hydraulic redistribution in a humid subtropical area, East China
URI https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fhyp.13643
https://www.proquest.com/docview/2350216282
https://www.proquest.com/docview/2400469251
Volume 34
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