3.7.2 Chemical processes

Grading statements — Physical, chemical, and ecological processes

Status
Very good
Very good

There are no significant changes in processes as a result of human activities.

Good
Good

There are some significant changes in processes as a result of human activities in some areas, but these are not to the extent that they are significantly affecting ecosystem functions.

Poor
Poor

There are substantial changes in processes as a result of human activities, and these are significantly affecting ecosystem functions in some areas.

Very poor
Very poor

There are substantial changes in processes across a wide area as a result of human activities, and ecosystem functions are seriously affected in much of the area.

or

Borderline

Borderline Indicates where a component or criterion is considered close to satisfying the adjacent grading statement.

Confidence

Confidence

Adequate high-quality evidence and high level of consensus

Limited evidence or limited consensus

Inferred, very limited evidence

Criterion and component summaries
Grade and trend
Confidence
Grade
Trend
Summary Heading
Chemical processes

The chemical processes within the Reef are generally in good condition. However nutrient cycling continues to be affected by land-based run-off. Ocean pH has decreased as a result of climate change.

Summary Heading
Nutrient cycling

Although substantial and ongoing changes to nutrient cycling since European settlement continue to affect inshore habitats, this process is understood to have been generally stable since 2019. There have been important advances in our understanding of nutrient cycling and in its integration into decision-making through improved models since 2019.

Summary Heading
Ocean pH

Ocean pH has declined within the Region, in line with global and Australian trends. It is likely that the rate of decline has increased in recent decades, driven by progressive ocean uptake of carbon dioxide due to increasing emissions. Ocean acidification has significant implications for coral reef ecosystems.

Summary Heading
Ocean salinity

Wider ocean patterns suggest that salinity may slowly increase in offshore areas within the Region, while inshore areas are subject to seasonal decreases in salinity as a result of freshwater input. Over the past 5 years, freshwater influence has been slightly above average overall with regional variation.