Abstract
Prescribed fire is an important tool for rangeland management in sage-steppe ecosystems, yet the long-term effects of this practice on soil hydraulic properties are not well known. We explore interactions among site geomorphology, soil organic carbon (SOC) soil N, soil water repellency (SWR), and plant community type on infiltration properties before fire and 8 years thereafter in a semiarid research watershed. The objective was to assess the sustainability of rangeland burning in sage-steppe ecosystems. Many types of measurements were made in three plant communities to identify how differences in soil hydraulic properties are related to differences in plant cover and soil texture and to determine relationships among SOC, SWR, soil water contact angle, and infiltration properties. Measurements were made on transects in burned and unburned catchments. We found that severity and occurrence of surface SWR were substantially reduced 8 years after a fire within the area originally covered with mountain big sagebrush, where the fire intensity was greatest. Surface SWR was lowest in the sparsely vegetated low sagebrush, where SOC was also lowest. Unsaturated hydraulic conductivity (Kh) increased in each vegetation type over the 8-year period after burning and was not directly related to SWR. Spatial variability in Kh was primarily controlled by soil texture, whereas differences in sorptivity (S) were controlled by SWR and aridity. SOC is not well correlated to soil surface SWR. The decadal scale changes in Kh and associations between S and site characteristics indicate forms of resilience to fire across a moisture gradient.
| Original language | English (US) |
|---|---|
| Journal | Water Resources Research |
| DOIs | |
| State | Accepted/In press - Jan 1 2018 |
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Keywords
- fire
- hydrology
- hydrophobic
- repellency
- SOC
- soil
ASJC Scopus subject areas
- Water Science and Technology
Cite this
Seasonal Wetness, Soil Organic Carbon, and Fire Influence Soil Hydrological Properties and Water Repellency in a Sagebrush-Steppe Ecosystem. / Chandler, David G; Cheng, Yang; Seyfried, Mark S.; Madsen, Matthew D.; Johnson, Chris E; Williams, C. Jason.
In: Water Resources Research, 01.01.2018.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Seasonal Wetness, Soil Organic Carbon, and Fire Influence Soil Hydrological Properties and Water Repellency in a Sagebrush-Steppe Ecosystem
AU - Chandler, David G
AU - Cheng, Yang
AU - Seyfried, Mark S.
AU - Madsen, Matthew D.
AU - Johnson, Chris E
AU - Williams, C. Jason
PY - 2018/1/1
Y1 - 2018/1/1
N2 - Prescribed fire is an important tool for rangeland management in sage-steppe ecosystems, yet the long-term effects of this practice on soil hydraulic properties are not well known. We explore interactions among site geomorphology, soil organic carbon (SOC) soil N, soil water repellency (SWR), and plant community type on infiltration properties before fire and 8 years thereafter in a semiarid research watershed. The objective was to assess the sustainability of rangeland burning in sage-steppe ecosystems. Many types of measurements were made in three plant communities to identify how differences in soil hydraulic properties are related to differences in plant cover and soil texture and to determine relationships among SOC, SWR, soil water contact angle, and infiltration properties. Measurements were made on transects in burned and unburned catchments. We found that severity and occurrence of surface SWR were substantially reduced 8 years after a fire within the area originally covered with mountain big sagebrush, where the fire intensity was greatest. Surface SWR was lowest in the sparsely vegetated low sagebrush, where SOC was also lowest. Unsaturated hydraulic conductivity (Kh) increased in each vegetation type over the 8-year period after burning and was not directly related to SWR. Spatial variability in Kh was primarily controlled by soil texture, whereas differences in sorptivity (S) were controlled by SWR and aridity. SOC is not well correlated to soil surface SWR. The decadal scale changes in Kh and associations between S and site characteristics indicate forms of resilience to fire across a moisture gradient.
AB - Prescribed fire is an important tool for rangeland management in sage-steppe ecosystems, yet the long-term effects of this practice on soil hydraulic properties are not well known. We explore interactions among site geomorphology, soil organic carbon (SOC) soil N, soil water repellency (SWR), and plant community type on infiltration properties before fire and 8 years thereafter in a semiarid research watershed. The objective was to assess the sustainability of rangeland burning in sage-steppe ecosystems. Many types of measurements were made in three plant communities to identify how differences in soil hydraulic properties are related to differences in plant cover and soil texture and to determine relationships among SOC, SWR, soil water contact angle, and infiltration properties. Measurements were made on transects in burned and unburned catchments. We found that severity and occurrence of surface SWR were substantially reduced 8 years after a fire within the area originally covered with mountain big sagebrush, where the fire intensity was greatest. Surface SWR was lowest in the sparsely vegetated low sagebrush, where SOC was also lowest. Unsaturated hydraulic conductivity (Kh) increased in each vegetation type over the 8-year period after burning and was not directly related to SWR. Spatial variability in Kh was primarily controlled by soil texture, whereas differences in sorptivity (S) were controlled by SWR and aridity. SOC is not well correlated to soil surface SWR. The decadal scale changes in Kh and associations between S and site characteristics indicate forms of resilience to fire across a moisture gradient.
KW - fire
KW - hydrology
KW - hydrophobic
KW - repellency
KW - SOC
KW - soil
UR - http://www.scopus.com/inward/record.url?scp=85055743105&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85055743105&partnerID=8YFLogxK
U2 - 10.1029/2017WR021567
DO - 10.1029/2017WR021567
M3 - Article
AN - SCOPUS:85055743105
JO - Water Resources Research
JF - Water Resources Research
SN - 0043-1397
ER -