Settlement FAQs

what is post settlement alluvium

by Lila Kuhic Published 3 years ago Updated 2 years ago
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Full Answer

A simple question can change the game

Howard Raiffa popularized the idea of the post-settlement settlement. When you get to an agreement, before you sign, ask the counterparty, “Is there any way that we could make this better for both of us?” You want to do so after an agreement has been reached. Why? Because the pressure is off, and you’re able to think more creatively.

Negotiation is about maximizing value

The essence of really good negotiation is maximizing value, right? Yet people don’t often go there. Because of this, they’re missing out on turning a good agreement into a great agreement.

Be mindful of your setup

The counterparty may think you’re trying to sneak something in or nickel and dime them, which is why the setup for your question is important. You need to make sure they know you’re comfortable with the agreement as it is. But you’re asking the question to see if there’s more value to be had for both parties.

How do floodplains store alluvium?

Floodplains store alluvium through lateral and vertical accretion, i.e. bedload deposits are being incorporated into the floodplain. Depositional episodes reflect the balance between the amount of sediments available and the capacity for it to be transported. Accordingly, the nature of LS on floodplains can be of different nature: (1) graded, when an excess of sediment and a deficit in transport capacity buries floodplains in continuous deposits, (2) cascading, when abundant sediment and limited transport capacity results in a series of frequent, but separated pockets, (3) punctuated, when limited sediment supply but efficient transport leads to deposition only in locally isolated pockets.

What is legacy sediment?

Legacy sediment (LS) is depositional bodies of sediment inherited from the increase of human activities since the Neolithic. These include a broad range of land use and land cover changes, such as agricultural clearance, lumbering and clearance of native vegetation, mining, road building, urbanization, as well as alterations brought to river systems in the form of dams and other engineering structures meant to control and regulate natural fluvial processes (erosion, deposition, lateral migration, meandering). The concept of LS is used in geomorphology, ecology, as well as in water quality and toxicological studies.

What are the most common contaminants that can absorb fine sediment?

The most common contaminants that can absorb fine sediment are trace metals, nutrients (e.g. nitrogen, phosphorus ), polynuclear aromatic hydrocarbons (PAHs), pathogens, polychlorinated biphenyls (PCBs), pesticides, volatile organic compounds (VOCs).

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When did sediment delivery and storage blossom?

of sediment delivery and storage that blossomed in the 1970s,

Is spatial deposition likely even without barriers?

1, abundant deposition and graded deposits are likely even without barriers or sinks. Thus, spatial

Does sediment have a long history?

sediment has a long history, although the deposits have

Does LS apply to sediment?

or urbanization. Moreover, LS should apply to sediment resulting from anthropogenic episodes on

Does sediment occur uniformly over the landscape?

sediment does not occur uniformly over the landscape

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Overview

Definitions

Definitions predominantly indicate post-settlement alluvium North America created as a result of agricultural clearance.
“Legacy Sediment (n.) Are sediments that (1) were eroded from upland slopes during several centuries of intensive land clearing, agriculture, and milling (in the eastern U.S., this occurred from the late 17th to late 19th Centuries); (2) collected along stream corridors and valley bottoms, bur…

Types and related landforms

LS encompasses sediment of differing structures and textures. They can be colluvial, containing poorly sorted, angular rock fragments deposited by mass wasting or sheet erosional processes, alluvial, containing well sorted, rounded clasts and very-fine grained suspended sediment deposited by fluvial processes.
Most LS is generated on highlands by erosional processes related to mass-wasting, sheet flow, ri…

Legacy effects

Scientific studies documenting the widespread alteration of sediment dynamics (i.e. sediment supply, sediment entrainment, transport, erosion, deposition and storage) by humans lead to the evidence that human activities have come to dominate erosional, depositional and geochemical processes in ecosystems. This is especially pronounced in river systems, given that rivers are the lowest topographic points of any landscape and consequently collect water, solutes, mineral sed…

See also

• Great Raft
• Vulnerable waters

Further reading

• Wohl, E. (2004). Disconnected Rivers: Linking Rivers to Landscapes. Yale University Press.
• Brierley, G., Fryirs, K. (2005). Geomorphology and River Management: Applications of the River Styles Framework. Blackwell Publishing.
• Wohl, E. (2014). Rivers in the Landscape: Science and Management. John Wiley & Sons, Ltd.

External links

• DamNation documentary: http://damnationfilm.com
• Chasing Water short documentary: https://vimeo.com/114386144
• National Geographic - Chasing Rivers: The Ganges: https://www.youtube.com/watch?v=mkPwEuflhKo&list=PLrNYY0nsrkqEY2qyGQJtln-c1Fy7kRoqs&index=2

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