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LAND3005
Course Profile
LAND3005
Soil Plant Relationships
School
of Land and Food Sciences
Date of this Course
Profile: February 2003
Changes since the previous version - 1.0
Units value
2
Class contact hours
three 1 h lectures, one 3 h practical, per week
Purpose of the course
“Soil Plant
Relationships” is intended to provide you with an understanding of the
inter-relationships between soil and plant growth. The subject material
is handled in a broad manner to provide students with interests in
ecological, environmental, and agricultural areas an understanding of
the role soil plays in plant growth. Key issues considered are the
supply of nutrient and water to plants. However, the course is
structured to provide students with an understanding of the underlying
mechanisms which control the interaction between plants and soil, rather
than providing a purely descriptive account.
Issues of chemical,
physical and biological fertility are considered, and the course aims to
integrate these various sub-disciplines into a coherent description of
plant growth in soil. This aim is enhanced through the use of a
substantial practical component where students undertake glasshouse
plant growth experiment. The practical component draws on the lecture
material, providing students with the opportunity to “see” the effects
of different soil treatments on plant growth, and the opportunity to
develop their understanding of the subject through informal interaction
with the lecturers and tutors.
Supply of plant
nutrients is considered from the perspective of the various reservoirs
of plant nutrients in the soil (organic matter, precipitated nutrient
forms, exchangeable nutrients, adsorbed nutrients). Individual
nutrients are considered to provide an example of the behaviour of a
broader class of nutrient elements; for example the behaviour of
nitrogen in the soil plant system is developed to describe the soil
organic matter as a pool of plant nutrients. Water supply to plants is
considered in detail, and interactions between water supply and nutrient
availability are discussed. Limitations to plant growth through
physical constraints, acidity and salinity are considered, and
approaches used for the remediation of these problems evaluated.
Staff
Assoc.
Prof. Neal Menzies
School of
Land and Food Sciences, St Lucia
Ph 07 3365
2059
Assoc.
Prof. Bing So.
School of
Land and Food Sciences, St Lucia
Ph 07 3365
2888
Course goals
Overall, our
expectation is that this course will,
·
provide you with a mechanistic
understanding of the process which buffer the supply of nutrients to
plants growing in soil.
·
develop your understanding of
the soil – plant – atmosphere continuum, including constraints to water
use through restriction of rooting volume by physical and chemical
constraints
·
introduce you to the use of
glasshouse plant growth experiments as a tool investigate soil – plant
relationships
·
enable you to describe soil
processes, and to predict the behaviour of soil systems on the basis of
your knowledge of the controlling processes.
As a graduate of
LAND3005 you will have
·
specific and detailed
understanding of the role of soil in supplying water and nutrients for
plant growth
·
sufficient knowledge of soil
attributes, and of their effect on plant growth, to permit you to identify
plant growth constraints across a broad range of settings
·
an appreciation of the
potential for manipulation of the soil system (either deliberate
manipulation – fertilizer use, or inadvertent manipulation – acid rain) to
affect the growth rates of plants
·
detailed knowledge of
glasshouse plant growth experimentation techniques.
Assumed background
Students are assumed
to have a basic knowledge of soil science (for example, completion of
LAND2003), and a basic knowledge of chemistry (at least high school
chemistry).
Teaching and learning
modes
The course is delivered as formal lectures
supported by practical sessions. Learning modules are available to
support some portions of the course.
Recommended
texts and references
“Introduction to Soil
Physics” by Daniel Hillel (Academic Press, Orlando) 1982 ISBN
0123485207)
“Physical Edaphology:
the physics of nonirrigated soils” by Sterling Taylor and Gaylen
Ashcroft (W.F. Freeman, San Francisco) 1972 ISBN 0716708183
“Russell’s Soil
Conditions and Plant Growth” edited by Alan Wild (Longman Scientific and
Technical, New York) 1988 ISBN 0582446775
Resources available and
required
Lecture notes are
available for some aspects of this course. These can be obtained from
the Soil Website (http://www.uq.edu.au/agsoil)
Assessment program
At the end of the
course we want you to have a clear understanding of the role soil plays
in plant growth. We consider that as professionals who will move into
widely differing work environments, you will put this knowledge to all
kinds of use. Indeed we hope that you use the opportunity to learn the
aspects of soil science that are most relevant to you; thus we expect
each student to pursue some aspects of the course in more detail than is
provided in the course notes, and to leave with a slightly different
knowledge set. However, there is a core set of knowledge that all of
you will need.
To assess this core
body of knowledge, you will sit a two-hour essay style examination at
the end of the semester. Past examination papers are available, and
these indicate the type of questions used. This examination represents
55% of the course mark. You are not permitted to use a dictionary in
the examination.
The practical
exercise is a major part of this course, and the written reports you
prepare will draw upon what you do in the practical, but also what you
have learned in the lectures and from your own reading. You will
prepare three suThe practical component is worth 45% of the course
total. Internal students will undertake a number of practical sessions
(information on these will be provided by your lecturer). External
students will undertake a residential school for the practical
component.
Assessment criteria
Practical reports are assessed primarily
on the basis that they demonstrate an understanding of the concepts
involved in the subject being discussed (50% of mark). Data
presentation appropriate to the arguments being made in the discussion
is considered important (30%) as is the use of appropriate literature
(10%). A small percentage of the assignment mark is attributed to the
layout, neatness, correct referencing, etc of the report (10%).
The final examination will be
marked solely on the basis that the answers demonstrate an understanding
of the subject matter.
Outcomes of
assessment exercises
The examination delivers a single mark
that is used in the calculation of your final grade. You will not be
provided with this mark, though it would be made available to you on
request. The practical exercises will be awarded a mark (to be used in
the calculation of your final grade) and will also be annotated with
comments to help you better understand the material assessed.
On the basis of this assessment material,
you will be awarded a grade on the 1 to 7 scale.
Formative and summative assessment
All practical reports and the final
examination will count toward your final grade.
The three submitted practical reports are
worth 15% each (a total of 45% for the practical component). The final
examination is worth 55%.
Required work
Lectures are provided
to help you learn the course content, but attendance at them is not
compulsory. You are welcome to learn from the course notes and
reference texts instead of attending lectures.
Practical exercises
must be attended in order to learn these techniques. Failure to attend
the practicals will result in the loss of part, or all, of the practical
component of the subject marks (45%). If you already have the knowledge
provided in the practical, a waiver to attendance can be negotiated with
the lecturing staff.
Assessment policies
The due date for submission of the
practical reports is final, unless a later submission time is negotiated
with the relevant staff member or tutor.
Plagiarism is
a serious issue of academic behaviour. The University’s policy on
plagiarism makes a comprehensive statement about the University’s
approach to plagiarism, the consequences and the principles associated
with preventing plagiarism. If you are in any doubt about the
University’s expectation of you in this regard, please visit the
following website.
http://www.uq.edu.au/hupp/contents/view.asp?s1=3&s2=40&s3=12
Support for
students with a disability
Any student with a
disability who may require alternative academic arrangements in the
course/program is encouraged to seek advice at the commencement of the
semester from a Disability Adviser at Student Support Services.
Course schedule 2003 -
LAND3005
Lect. Date Lecturer Content
|
1 |
3/3 |
NWM |
|
Subject overview, assessment, practical component. |
|
2 |
4/3 |
NWM |
N1 |
Mineralogy |
|
3 |
7/3 |
HBS |
B1 |
Soil as a medium for Plant
Growth |
|
4 |
10/3 |
HBS |
B2 |
Soil Texture/Particle size
distribution |
|
5 |
11/3 |
NWM |
N2 |
Organic matter in soils. |
|
6 |
14/3 |
HBS |
B3 |
Relevance and
characteristics associated with texture |
|
7 |
17/3 |
HBS |
B4 |
Soil water interactions :
water content vs potentials |
|
8 |
18/3 |
NWM |
N3 |
Organic matter as a pool of plant nutrients |
|
9 |
21/3 |
HBS |
B5 |
Soil water interactions :
water potential components |
|
10 |
24/3 |
HBS |
B6 |
Soil water interactions :
soil water characteristics |
|
11 |
25/3 |
NWM |
N4 |
Organic matter as a source of plant nutrients |
|
12 |
28/3 |
HBS |
B7 |
Movement of water:saturated
soils and hyd. Conductivites |
|
13 |
31/3 |
HBS |
B8 |
Movement of water in soils :
unsaturated soils |
|
14 |
1/4 |
NWM |
N5 |
Solubility relationships – solubility of rock phosphate |
|
15 |
4/4 |
HBS |
B9 |
Water uptake by plants |
|
16 |
7/4 |
HBS |
B10 |
Field processes of
infiltration, evaporation and redistribution |
|
17 |
8/4 |
NWM |
N6 |
Ion exchange – plant nutrients and effects of acidification |
|
18 |
11/4 |
HBS |
B11 |
Soil Structure :
arrangements of particles into aggregates |
|
19 |
14/4 |
HBS |
B12 |
Soil structure : cations and
the diffuse doule layers |
|
20 |
15/4 |
NWM |
N7 |
Adsorption – underlying theory and description |
|
21 |
28/4 |
NWM |
N8 |
Nitrogen |
|
22 |
29/4 |
NWM |
N9 |
Nitrogen |
|
23 |
2/5 |
HBS |
B13 |
Soil structure |
|
24 |
6/5 |
NWM |
N10 |
Phosphorus |
|
25 |
9/5 |
HBS |
B14 |
Soil Structure : soil
consistency and tillage |
|
26 |
12/5 |
NWM |
N11 |
Potassium, Calcium, Magnesium |
|
27 |
13/5 |
NWM |
N12 |
Sulphur |
|
28 |
16/5 |
HBS |
B15 |
Consequences of structural
degradation |
|
29 |
19/5 |
NWM |
N13 |
Micronutrients – deficiency |
|
30 |
20/5 |
NWM |
N14 |
Micronutrients – toxicity |
|
31 |
23/5 |
HBS |
B16 |
Soil Management : surface
soils |
|
32 |
26/5 |
NWM |
N15 |
Soil Testing |
|
33 |
27/5 |
NWM |
N16 |
Waterlogged soils |
|
34 |
30/5 |
HBS |
B17 |
Soil Management : subsurface
soils |
|
35 |
2/6 |
NWM |
N17 |
Acidity |
|
36 |
3/6 |
NWM |
N18 |
Salinity / sodicity |
|
37 |
6/5 |
HBS |
B18 |
Management of Vertisols |
|