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SSooiill iiss ccoommppoosseedd ooff:: 
 rock particles 
 humus 
 mineral salts 
 water 
 air 
 organisms
RRoocckk ppaarrttiicclleess 
vary in size 
Gravel Sand Silt Clay
TThhrreeee ttyyppeess ooff SSooiill:: 
Clay Sandy 
Loam 
BBEESSTT 
TTYYPPEE
TThhrreeee ttyyppeess ooff ssooiill::-- 
22 SSaanndd :: 11 CCllaayy
CCllaayy SSooiill:: 
 heavy soil 
 difficult to dig as clay sticks
CCllaayy SSooiill:: 
 when dry it forms hard clods 
 little air present 
Clay Sandy 
Loam
CCllaayy SSooiill:: 
retains water 
soil becomes waterlogged
A waterlogged soil has few air 
spaces as these become filled with 
water
PPaarrttiiccllee ssiizzee aaffffeeccttss tthhee 
ffoolllloowwiinngg pprrooppeerrttiieess ooff ssooiill::-- 
1. amount of air
PPaarrttiiccllee ssiizzee aaffffeeccttss tthhee 
ffoolllloowwiinngg pprrooppeerrttiieess ooff ssooiill::-- 
2. the rate and amount of drainage
3. the rise of 
water in the 
soil 
(capillarity) 
CCaappiillllaarryy wwaatteerr
The smaller the particle size, 
the higher water rises.
QQuueessttiioonn:: [[AAPPRRIILL,, 22001100]] 
PPaappeerr 22BB 
List TWO properties of soil that 
are affected by soil texture. (4) 
 The distance between soil particles 
 The amount of air between soil 
crumbs/drainage 
 The rise of water in the soil 
(capillarity) 
Any TWO
CCllaayy SSooiill iiss mmaaddee lliigghhtteerr bbyy 
aaddddiinngg::-- 
i) humus 
How do these work? 
ii) lime
AAddddiinngg 
lliimmee
CClluummppiinngg ooff ssooiill ppaarrttiicclleess 
iinnttrroodduucceess aaiirr iinn ssooiill 
A clay soil 
before 
treatment. 
lime 
humus 
A clay soil after 
treatment.
GGoooodd ccrruummbb ssttrruuccttuurree 
[[tteexxttuurree]] ooff ssooiill
WWhhaatt iiss ‘‘hhuummuuss’’?? 
black or dark brown material that 
remains after decomposition
DDaarrkk ssooiill:: rriicchh iinn hhuummuuss
0-45cm 
45-90cm 
Bedrock 
Upper topsoil layer is 
dark. Why? 
Lower soil layer is rich 
Lower soil layer is rich 
in salts. Why? 
in salts. Why?
QQuueessttiioonn:: [[AAPPRRIILL,, 22001100]] PPaappeerr 22BB 
Explain how humus: 
i) Increases the soil’s water 
content. (2) 
Absorbing large amounts of water 
or reducing evaporation from the 
soil.
QQuueessttiioonn:: [[AAPPRRIILL,, 22001100]] PPaappeerr 22BB 
b. Explain how humus: 
ii) Improves the texture of a clay 
soil. (2) 
Humus helps soil particles 
stick together into larger crumbs.
SSaannddyy SSooiill:: 
 light soil 
 water drains quickly 
As water drains 
quickly TWO 
disadvantages 
result:
11.. SSooiill ddrriieess uupp qquuiicckkllyy 
Why is this a disadvantage for the 
farmer? 
Water is expensive!!
22.. SSaallttss aarree lleeaacchheedd eeaassiillyy 
LLeeaacchhiinngg:: 
ssaallttss ddiissssoollvvee && 
aarree lloosstt
SSaannddyy SSooiill iiss iimmpprroovveedd bbyy:: 
adding humus as this:- 
1.holds more water 
2.provides salts
SSooiill iiss ccoommppoosseedd ooff:: 
 rock particles 
 humus 
 mineral salts 
 water 
 air 
 organisms
HHuummuuss 
a jam-like substance made up of 
decayed plants and animals 
is found in the topsoil 
– blackish in colour
HHuummuuss 
if there is not enough oxygen, 
materials accumulate to form 
half decayed materials called 
peat 
peat decays into humus if placed 
in well aerated soil
HHuummuuss 
helps to clump soil particles into 
crumbs
HHuummuuss iimmpprroovveess ssooiill bbyy::-- 
providing mineral salts from 
decay by bacteria and fungi 
providing air spaces 
retaining water 
improves crumb structure 
(prevents soil from being blown 
away)
LLooaamm SSooiill 
ccoonnttaaiinnss ttwwiiccee aass mmuucchh ssaanndd aass 
ccllaayy 
Clay [1 part] 
Sand [2 parts] 
silt
HHooww ccaann yyoouu 
sseeppaarraattee tthhee ssooiill 
ppaarrttiicclleess aass sshhoowwnn 
iinn tthhee cchhaarrtt?? 
 add water 
 mix 
 leave to 
settle
EExxppeerriimmeenntt 
To find the components of 
soil.
EExxppeerriimmeenntt 
To find the organic content of 
soil.
percentage of organic matter = 
loss in weight ´ 
weight of original dry sample 
100 
Original weight: 105 g 
Final weight: 100 g 
Loss in weight: 5 g 
5 ´100 = 4.8% 
105
SSOOIILL 
 rock particles 
 humus 
 mineral salts 
 water 
 air 
 organisms
WWaatteerr 
is found as thin films around soil 
particles 
water moves 
upwards towards 
the surface by 
capillarity
EExxppeerriimmeenntt 
To find the water content of 
soil.
PPrreeccaauuttiioonn wwhheenn hheeaattiinngg ssooiill:: 
Temperature must NOT be more 
than 100°C. 
WHY?
PPeerrcceennttaaggee ooff wwaatteerr iinn ssooiill:: 
loss in weight ´ 
original wet sample 
100 
Original wet weight: 200 g 
Final weight: 185 g 
Loss in weight: 15 g 
15 ´100 = 7.5% 
200
SSOOIILL 
 rock particles 
 humus 
 mineral salts 
 water 
 air 
 organisms
TTWWOO ssoouurrcceess ooff ssaallttss iinn ssooiill:: 
1. rock erosion 
2. decay of dead organisms
SSaalliinniissaattiioonn iiss aa SSooiill PPrroobblleemm 
 gradual accumulation of salt in the soil, usually due to 
improper irrigation techniques 
 often in arid and semi-arid 
areas (natural mineral salt 
conc. high) 
– The little precipitation that 
falls is quickly evaporated 
– Leaves behind salts 
 salt concentrations get to 
levels toxic to plants
MMaannyy oorrggaanniissmmss bbrriinngg aabboouutt 
ddeeccaayy::
EExxppeerriimmeenntt 
To compare the drainage of two 
soil samples.
SSOOIILL 
 rock particles 
 humus 
 mineral salts 
 water 
 air 
 organisms
AAiirr iiss uusseedd bbyy:: 
1. roots for 
respiration 
2. decomposers to 
decay material into 
humus
A good ssooiill hhaass aa lloott ooff aaiirr 
ssppaacceess bbeettwweeeenn tthhee ccrruummbbss 
How can a 
farmer 
introduce 
air into 
the soil?
By ploughing
EExxppeerriimmeenntt 
To estimate the volume of air in a 
soil.
EExxppeerriimmeenntt 
percentage of air = volume of air in soil 
volume of soil sample 
´ 100 
Conclusion: 
 Air is important in soil for roots to respire 
and for decomposers to remain alive.
 rock particles 
 humus 
 mineral salts 
 water 
 air 
 organisms 
SSOOIILL
BBaacctteerriiaa && FFuunnggii 
make salts 
available to 
plants
EEaarrtthhwwoorrmmss iimmpprroovvee ssooiill bbyy:: 
1. their burrows they mix and loosen the soil 
and so help to drain and aerate it 
2. providing salts due to their wastes and by 
pulling leaves into the soil
EEaarrtthhwwoorrmmss iimmpprroovvee ssooiill bbyy:: 
3. making the soil alkaline as it passes 
through their intestine – bacterial growth is 
favoured by this pH
EEaarrtthhwwoorrmmss iimmpprroovvee ssooiill bbyy:: 
4. binding soil particles together by the 
secretions from the intestines 
5. making the soil finer – young roots can 
emerge easier
HHaarrmmffuull OOrrggaanniissmmss 
Nematodes can be harmful by:- 
1.feeding on bacteria 
2.being ectoparasites and pierce 
root 
3.being endoparasites and damage 
roots and crops
HHaarrmmffuull OOrrggaanniissmmss 
various insect larvae eat the 
roots of plants e.g. wireworms 
(beetle larvae)
SSooiill ffeerrttiilliittyy ccaann bbee iinnccrreeaasseedd 
bbyy:: 
1. Adding fertilisers 
2. Crop rotation 
3. Ploughing 
4. Keeping a neutral pH
TTwwoo ttyyppeess ooff SSooiill FFeerrttiilliisseerr 
1. Natural fertilisers 
2. Artificial / 
Chemical fertilisers
NNaattuurraall FFeerrttiilliisseerrss 
Animal manure 
Compost
WWhhyy iiss tthhee tteemmppeerraattuurree aatt tthhee 
cceennttrree ooff tthhee ccoommppoosstt ppiillee 
hhiigghheerr tthhaann aammbbiieenntt 
tteemmppeerraattuurree??
Heat released by microbes is 
difficult to be lost to the 
surroundings – far from surface. 
Cool 
air in 
Cool 
air in 
Warm air out
AAddvvaannttaaggeess ooff NNaattuurraall 
FFeerrttiilliisseerrss 
provide a wide variety of salts 
maintain the crumb structure 
long-lasting
DDiissaaddvvaannttaaggeess ooff NNaattuurraall 
FFeerrttiilliisseerrss 
Salts are released slowly – decay is 
slow 
Bad smell 
Pests can grow in it
AArrttiiffiicciiaall FFeerrttiilliisseerrss 
Manufactured from chemical 
compounds
AAddvvaannttaaggeess ooff AArrttiiffiicciiaall 
FFeerrttiilliisseerrss 
Salts are very soluble and are quickly 
available to the plant 
No pests in it 
No unpleasant smell
DDiissaaddvvaannttaaggeess ooff AArrttiiffiicciiaall 
FFeerrttiilliisseerrss 
salts are leached quickly 
destroy the crumb structure (soil 
becomes a powder)
DDiissaaddvvaannttaaggeess ooff AArrttiiffiicciiaall 
FFeerrttiilliisseerrss 
have less types of salts than manure 
no water-holding capacity
DDeessccrriibbee wwhhaatt mmaayy hhaappppeenn ttoo aa ssooiill wwhheenn 
oonnllyy cchheemmiiccaall 
ffeerrttiilliizzeerrss aarree uusseedd oovveerr aa lloonngg ttiimmee ppeerriioodd.. 
loss of soil humus/organic matter content; 
loss of soil texture/crumb structure; 
impaired soil drainage/waterlogging; 
loss of aeration; 
Good 
crumb 
structure 
Bad 
crumb 
structure
QQuueessttiioonn:: [[SSEEPP,, 22001111]] PPaappeerr 22 
List TWO types of natural fertiliser. 
(2) 
1. Compost / peat 
2. Animal manure
QQuueessttiioonn:: [[MMAAYY,, 22001111]] PPaappeerr 11 
Give the biological explanation of the 
message in the following poster. (3) 
Decomposers, consisting of 
bacteria and fungi, bring 
about the decay of the dead 
plant material. The decaying 
material is called compost 
and is vital for the growth of 
plants as mineral ions are 
released into the soil. Plants 
use nitrates, phosphates and 
other mineral salts to keep 
healthy.
SSooiill ffeerrttiilliittyy ccaann bbee iinnccrreeaasseedd 
bbyy:: 
1. Adding fertilisers 
2. Crop rotation 
3. Ploughing 
4. Keeping a neutral pH
CCrroopp rroottaattiioonn 
means the planned order of specific 
crops planted on the same field 
 rotation may vary from 2 or 3 year or 
longer period 
 e.g. 
- wheat in autumn 
- root crop in summer 
- barley or oats in spring 
- leguminous plants (clover, peas)
if the same crop is planted: 
certain salts are depleted
BBeenneeffiittss ooff CCrroopp 
rroottaattiioonn 
1. maintains crumb structure 
2. supplies nitrates 
3. reduces infection to plants as a 
pest cannot continue its life cycle if 
a different crop is planted
SSooiill ffeerrttiilliittyy ccaann bbee iinnccrreeaasseedd 
bbyy:: 
1. Adding fertilisers 
2. Crop rotation 
3. Ploughing 
4. Keeping a neutral pH
Beneficial effects of ploughing: 
makes soil porous so water drains 
better 
 introduces air into the soil
Beneficial effects of ploughing: 
 incorporates the residue from the 
previous crop into the soil 
 reduces the prevalence of weeds in 
the fields
TTHHEE EENNDD

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