Related Experiment Video
Updated: Mar 18, 2026

06:42
Measuring Phosphorus Release in Laboratory Microcosms for Water Quality Assessment
Published on: July 22, 2019
7.2K
Stream channel storage: Closing the watershed total phosphorus budget
William J Beck1, John L Kovar2, Thomas M Isenhart1
1Department of Natural Resource Ecology and Management, Iowa State University, Ames, Iowa, USA.
Journal of Environmental Quality
|March 17, 2026
Summary
In agricultural watersheds, remobilized phosphorus from in-channel sediments is the primary source of annual total phosphorus (TP) loads, not streambanks. Restoring watershed hydrology and floodplain connectivity is key to reducing TP loads.
Area of Science:
- Environmental Science
- Hydrology
- Agricultural Science
Background:
- Total phosphorus (TP) loading from agricultural watersheds is a significant environmental concern.
- Quantifying in-channel sediment contributions to TP loads is challenging but crucial for effective management.
- Walnut Creek watershed in Iowa serves as a case study for understanding phosphorus dynamics in agricultural landscapes.
Purpose of the Study:
- To develop a 3-year total phosphorus budget for the Walnut Creek watershed.
- To estimate the contribution of in-channel storage to annual TP loads.
- To identify key sources and pathways of TP export from the watershed.
Main Methods:
- Constructed a comprehensive TP budget using data on streambank erosion, overland flow, baseflow, and floodplain flux.
- Quantified phosphorus contributions from various sources including in-channel sediment remobilization.
- Analyzed the influence of hydrological conditions, including drought and high-discharge events, on TP loads.
Main Results:
- Remobilization of sediment-bound phosphorus from in-channel storage was the dominant contributor to annual TP loads.
- Overland flow was the second largest contributor to TP loads.
- Streambank erosion contributed minimally, and baseflow dissolved phosphorus was significant in drought years.
- Floodplain storage was negligible due to low peak flows and channel incision but represents a significant storage opportunity.
Conclusions:
- In-channel sediment P remobilization is the primary driver of annual TP loads in this agricultural watershed.
- Reducing peak flows through watershed hydrology restoration and enhancing channel-floodplain connectivity are critical for mitigating TP loads.
- Future climate scenarios and channel evolution may increase the impact of high-discharge events on TP export.
More Related Videos
Related Concept Videos
The Phosphorus Cycle
44.8K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
44.8K
Factors Affecting Solubility
38.0K
Compared with pure water, the solubility of an ionic compound is less in aqueous solutions containing a common ion (one also produced by dissolution of the ionic compound). This is an example of a phenomenon known as the common ion effect, which is a consequence of the law of mass action that may be explained using Le Chȃtelier’s principle. Consider the dissolution of silver iodide:
38.0K
Design Example: Analyzing Capacity Contours for Flood Risk Assessment
349
Flood risk assessment involves careful planning and analysis to ensure the safety of communities near water retention structures. Capacity contours are a vital tool in this process, as they illustrate the potential spread of water at specific levels in a given area. In the context of building a bund across a small valley, these contours play a critical role in evaluating the safety of nearby residential areas.In this example, the bund is intended to store stormwater in the valley. The engineers...
349
Net Change Theorem
113
The Net Change Theorem is a fundamental principle in calculus that establishes a direct relationship between a function’s rate of change and its accumulated change over an interval. Mathematically, it states that the definite integral of a function's derivative over a given interval [a,b] yields the net change in the original function:This theorem has significant applications in various real-world scenarios, including physics, economics, and engineering. A particularly useful application...
113

