General Flashcards

1
Q

Accessibility of nutrients - Mass flow

A

Mass flow is the movement of dissolved ions withthe flow of water (water is flowing into the plant as water moves upwards by evaporation, and into the root by transpiration - water is therefore flowing and has ions in it). Sometimes this is enough, sometimes it isn’t

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2
Q

Accessibility of nutrients - diffusion

A

Movement from high to low concentrations, to equalise concentration gradients. If plant is taking out nutrients faster than mass flow replenishes them, thenthere is a depletion zone around the root (i.e. if uptake> replenishment) - leads to depletion (e.g. P, Zn).

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3
Q

Accessibility of nutrients - interception (by roots)

A

Root growth towards nutrients. Depends on:

  • How much roots expand through the soil
  • Efficiency of absorption by root haris

But, for e.g. P, don’t get enough by this method alone

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4
Q

Distance moved by diffusion

A

The distance a nutrient can move by diffusion will increase with increasing soil water content. With increased water content, nutrients such as K+, NO3- can take straight path. If water content low, pathway longer (tortuosity). NO3- moves furthers because nearl all of it is in solution, whereas other compounds are on exchange sites, or sorbed tightly

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5
Q

Accesibility of nutrients - relative importance varies

A
  • P not much in soil solution, so mass flow low, relies heavily on diffusion
  • With Ca, Mg, Su, N lots in solution, so lots of mass flow
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6
Q

Soil physical properties which affect movement of water and nutrients

A
  • Texture - particle size distribution, surface area
  • Structure - paths for water and air movement, root growth and nutrient movement. Biological activity 0 if you change amount of water, you also change how quickly microbes move nutrients between pools
  • Structural stability - confers resistance to structural breakdown by rainfall and tillage. (surface crusts, impeded water infiltration, runoff, erosion)
  • Soil strength - (affects penetration of roots)
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7
Q

how does soil minimise changes in soil solution chemistry?

A

Buffering using CEC. When cation added, it quickly equilibrates with exchange cations, removing K+ solutions from solution. If plant removes cation, it is replenished from cation exchange site pool

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8
Q

How is soil pH buffered?

A

__

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9
Q

For CEC and pH buffering what soil components contributed most to CEC?

A

__

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10
Q

Plants access nutrients via 3 methods?

A

interception, mass flow, diffusion

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11
Q

Soil physical properties play important role in chemical fertility through:

A
  • Effect on root growth (soil strength)
  • Aeration (number and size of pores)
  • Water movement
  • Erosion
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12
Q

Soil fertility

What is the concentration called at which yield is maximised?

A

the lower critical concentration

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13
Q

Soil fertility

Will a deficiency of non essential elements result in a decrease in crop yield/ plant growth?

A

No, for non essential elements only have second part of graph. Only problem is potential toxicity, plants can grow to maximum without these elements. At the ‘critical concentration’ the concentration of a non essential element (or essential element) becomes too high, and the yield decreases due to toxicity

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14
Q

Micronutrients (trace elements)

A

__

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15
Q

The availability of most trace metals is low at a pH of 8 because their hydroxide salts are very insoluble?

A

____

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16
Q

The availability of soil macro nutrients (N,P,K) is more important than the availability of soil micronutrients (e.g. trace metals)

A

__

17
Q

Micronutrients

Transition metals

A
  • most have 2+ charge, and are in active sites that allow reactions to take place at a quicker rate
18
Q

Micronutrients

A

Transition metals, B, Se, Na, Cl

19
Q

Definition of essential element

A

An element is not considered essential unless deficiency of it makes it impossible for a plant to complete its lifecycle

20
Q

Are non essential elements directly involved in nutrition of plant?

A

No

21
Q

Toxicity

A

sTrong correlation between concentration of element in soil and concentration in plant. Hard to exclude, b/c often use similar pathways of similar elements (eg Cd for Zn)

22
Q

Fertilisers source of trace elements (essential and non essential)

A
  • Cd in P fertilisers

- Lead in N and K fertilisers

23
Q

Is labile pool immediately available?

A

No, has to come off exchange sites and move into soil solution

24
Q

N availability

A

at pH 7 rapid conversion by microbes from ammonium to nitrate. Microbes happiest at 6-8. As you move from that range N decreases

25
Q

P availiability

A

Fixed at low pH by rxn with Fe and Al oxides, and at high pH by precipitation of Ca phosphates

26
Q

K, Ca, Mg base cation availability

A

NOt available at low pH b/c leached from soils

27
Q

Fe, Mn, Al availability

A

V soluble under acidic conditions, so can be toxic. But when you increase pH form Mn and Fe oxides. Quite insoluble. Move to stable pool (low solubility of hydroxide salts)

28
Q

B availaiblity

A

dry conditions goes into solution, wet conditions gets leached (so low availiabiltiy in low pH soils)

29
Q

Alkalinity - Fe, P

A

Due to hydrolysis of carbonates, get OH-, so Fe and P precipitate out (can be problem)

30
Q

CaCO3, Mg CO3 effect of addition

A

CO32- + H2O = HCO-3 + OH- . This reaction driven in forward direction, so more OH- produced and pH goes up

31
Q

Alkaline soils >8.5 indicates presence of::

A

Substantial quantities of MgCO3, Na2CO3. CaCO3 most common. Low availability of P and Fe are common problems in alkaline soils

32
Q

Potential exam q. How would you measure paddock? 3 methods.

A

+Random sampling - removes poss of subjective bias, but doesn’t identify clear areas of variation (e.g vegetation)

Choose 2 diff zones, sample w/in to account for variation in vegetation. Deterimine depth (eg top 10cm for P and N). Representative samples, so avoid random big boulder)

Sample processing after collection:

  • to dry or not to dry
  • Grinding/ sieving - adv is homogenisation, disadv is changes to property