chapter 4c Flashcards

1
Q

more H+ ions

A

pH low (acidic)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

more OH+ ions

A

pH high (alkalinity)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

negative logarithm of the total hydrogen ion concentration in the solution

A

pH

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

acidity or alkalinity, due to relative concentration of H+ and OH ions

A

pH

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

humid
arid
inorganic

A

5 to 7
7 to 9
4 to 10

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

relationship between pH and %BS

A

linear relationship

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

as pH increases

A

H+ decreases

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

method by pH meter, more accurate

A

electrometric method

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

organic dyes, litmus paper (ex: cornell pH)

A

colorimetric method

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

soil test kit

A

nitrogen, phosphorus, and potassium. next is lime requirement

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

effects of soil pH on microbial act

A

fungi: unaffected
bacteria & actinomycetes: inhibited at pH 5

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

(1) origin of soil acidity

A

release of hydrogen atoms under natural chemical processes in the soil

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

rel of H under natural chem

A

*atmospheric carbon dioxide reacts w/ water to form carbonic acid
*organic molecules reacts w/ water and causes acid dissociation
*oxidation of ammonium nitrogen, sulfur, and iron

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

(2) origins of soil acidity

A

accumulation of OM and subsequent release of products of decomposition: fulvic and humic acid

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

(3) origins of soil acidity

A

reaction of aluminum cations with water, “hydrolysis”

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

(4) origins of soil acidity

A

natural deposition
- lightning deposits nitric acid
- volcanic activity deposits sulfuric acid
- mineral weathering: Pyrite or Fool’s Gold (FeS2) once oxidized, results to formation of acid sulfate soils

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

(5) origins of soil acidity

A

human factors
- oxidation of applied synthetic ammonium-based fertilizer
-oxidation of nitrogen compounds in applied animal manure or sewage
- deposition of acid rain (nitric and sulfuric caused by industrialization)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

forms of soil acidity

A

active acidity: due to H+ in soil solution, determined as pH
reserve acidity: due to H+ and Al+++ in the solid phase

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

ability of soil to resist sudden/drastic changes in pH

A

buffering capacity

20
Q

measure of the buffering capacity of soil

A

reserve and active acidity

21
Q

buffering capacity is high if

A

CEC is high
clay content is high
OM content is high

22
Q

production constraints associated with acid soils

A

aluminum toxicity- usually damages the root system first
mn toxicity- less common than Al toxicity
nutrient deficiency- P, Ca, and Mo deficiency (also nitrogen)

23
Q

(4-5) production constraints with acid soils

A

restricted microbial activities: mineralization of organic N, biological fixation of N
incidence of plant diseases: some plants are more likely to be affected by damping off (fungal disease) and root rot in acid soils

24
Q

(1) management strategy

A

reduce acidification
- minimize use of acidifying fertilizer
- reduce leaching of N by use of split applications of fertilizer
- return plant material to soil

25
(2) management strategy
used acid-tolerant crops - sweet potato, coffee, radish, tomato, pineapple, strawberry, irish potato
26
(3-4) management strategy
apply more nutrients apply agricultural lime
27
only means of correcting soil acidity
lime
28
any oxide, hydroxide, or carbonate of Ca or Mg used to neutralize soil acidity
lime
29
carbonate form
CaCo3 (calcitic limestone) CaMg(Co3)2 dolomitic limestone
30
oxide and hydroxide form
CaO (burned lime) Ca(OH)2 hydrated lime
31
depends on soil
pH: lower- more lime exchangeable Al- more, more lime texture- clayey, more lime OM- depeds
31
amount of lime depends on soil
pH: lower- more lime exchangeable Al- more, more lime texture- clayey, more lime OM- depends
32
amount of lime depends on (2)
type and variety of crops to be grown
33
amount of lime depends on (3)
kind of lime - fineness - chemical guarantee
34
amount of lime depends on (4)
economic return from lime application
35
amount of salt that have accumulated in the soil
salinity
36
expressions of chemical guarantee of lime
oxide content in %CaO r %MgO calcium oxide equivalent- strength in pure CaO calcium carbonate equivalent (neutralizing power)- CaCo3
37
high osmotic potential
low salt concentration
38
low osmotic potential
high salt concentration
39
excess Na causes
disperse and swell, affect drainage, aeration, and root penetration. toxicity to plants
40
ability of substance to conduct electric current
electrical conductivity
41
ability of an electrolytic solution to conduct electric current
electrical conductivity
42
index of total ionic concentration in solution
electrical conductivity
43
more saline
higher EC
44
correct salinity
irrigation water
45
correct sodicity
gypsum or sulfur