Variable Soil Moisture Responses to Rainfall Events in Fields under Different Management Practices

Amila Ljutic, Jack Moore,Genevieve Ali,Laura Van Eerd,Merrin L. Macrae,Claudia Wagner-Riddle

Hydrological Processes（2024）SCI 3区SCI 2区

Univ Guelph

Cited 0|Views3

Abstract

Soil moisture response to rainfall is a key factor that dictates how well a landscape can support crop growth as well as its susceptibility to water runoff and leaching, however, few studies have investigated how agricultural management impacts this important soil function. This study compares two common agricultural soil treatments (cover crops and soil compaction) and their soil moisture response to rainfall in comparison to a control. In a humid temperate climate during March to November, individual rainfall events were delineated over two growing seasons and corresponding soil moisture responses were identified using in situ soil moisture sensors at four soil depths (20, 30, 40, and 60 cm). Results suggest that hydrological responses differed with both event type and management treatment. Not all rainfall events triggered a response: those that triggered responses at shallower soil depths were typically characterized by higher total event rainfall, and higher maximum and average rainfall intensity. In contrast, rainfall events triggering responses at deeper soil depths were characterized by longer event duration as well as higher 10-day antecedent rainfall (AR). Soil moisture responses for the cover crop treatment were characterized by relatively lower initial and peak soil moisture at shallower depths but higher values at 60 cm depth, whereas soil moisture responses for the control and compacted soil treatments demonstrated the opposite. Matrix flow was most often generated for rainfall events with high magnitude and was not preferentially associated with any particular soil treatment. However, specific conditions were needed to generate vertical preferential flow, namely high total event rainfall for both horizons, or high AR for preferential flow in the Ap horizon, or high rainfall intensity for preferential flow in the Bt horizon. Our findings demonstrate the potential for detailed event-based soil water process analysis using high-frequency, multi-depth soil moisture data. Rainfall events that triggered a soil moisture response had significantly different duration, size, and intensity than those that did not trigger a soil moisture response. While antecedent rainfall played a role in promoting both matrix and preferential flow, at least 20 mm of cumulative rainfall was required to generate preferential flow. Overall, control plots had the highest number of soil moisture responses to rainfall, followed by the cover-cropped plots and the compacted plots. image

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Key words

cover crops,matrix flow,preferential flow,rainfall events,soil compaction,soil moisture

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