Biotechnology Commission (AEBC) Research Agendas Workstream
Meeting 26 November 2004
Paper RA5.1: A Brief Commentary on Soil Science Developments – A Paper to Stimulate Discussion by Jeff
Maxwell
Introduction and Summary
The soil is a highly complex and dynamic system. Understanding its physical and chemical properties
is hard enough, but it also harbours a remarkable biodiversity. The relationships between these abiotic
and biotic components and the soil’s many functions are still poorly understood. Nevertheless, since its
beginnings in the 19th century, soil science has helped to produce the vastly improved yields of modern
agriculture.
The soil’s role in a host of other processes, such as carbon cycling and climate change, pollution
and ecosystem function mean that factors other than a desire to improve agricultural productivity can
influence research agendas. In the last twenty five years, the key drivers behind soil science have
changed considerably as technical advances have begun to allow fundamental soil processes to be
understood. Soil science is an interesting case study of how a particular area of science is adapting to
changing priorities and as technical developments allow new approaches to be taken.
The Nineteenth Century
The early stages of soil science from the beginning to the late 19th century developed along two
separate lines – the agricultural soil chemistry path and the weathered rock, soil physics and
agrogeology path (1). There was little significant interaction between them until the
beginning of the 20th century. However, there were a number of important developments over this period:
Liebig’s mineral theory of plant nutrients of the 1840’s; the recognition of the importance of the soil
profile (later pedon) by Darwin and Dokuchaev; the identification of soil forming processes (e.g. the
role of earthworms in soil mixing, Darwin 1881); the variable nature of humus (soil organic matter) and
its role in soil forming processes (e.g. Mueller, 1840-1926);
Consequent upon and following the establishment of the long-term field experiments by Lawes and
Gilbert in the 1840’s the research at Rothamsted focussed on the relationship between soil conditions
and fertility and its effect on crop yield. Out of these experiments and many others the first edition
of Soil Conditions and Plant Growth by Sir E John Russell was published in 1912. His son, Walter Russell,
published the eighth edition in 1973, and the 11th multi-authored edition was published in 1988. The
several editions of this book have played no small part in shaping the evolution of soil science in
Britain and in many other countries of the world (2) recognising that soil science and
soil management is a multi-disciplined activity embracing pedology, soil chemistry, soil physics, soil
biology, plant nutrition and other branches of the life sciences.
The principle drivers of research during the 19th century were curiosity and a need to
understand how to use soils and fertilise them to maintain and increase crop yields. The design of the
long-term Rothamsted experiments reflects this; a comparison of the yield of crops grown on soils
receiving farm yard manure plus inorganic nitrogen and soils receiving inorganic nitrogen, phosphorus
and potassium compound fertilisers. The funding came from trusts and farmers committed to improving
their husbandry techniques and the output from their farms. Farmers were involved in the research.
The Twentieth Century
At the beginning of the 20th century an understanding of the role of microbes in the decomposition of
plant residues in returning nutrients to the soil (e.g. Waksman, 1888-1973) was developed, and towards
the middle of the century following Jenny’s model (1941) of soil nutrient dynamics, different types of
model were developed to understand the medium and long term dynamics of soil organic matter. The early
part of the 20th century saw also the beginnings of soil survey in Britain which led ultimately to the
production of the 1:250,000 scale soil survey of England and Wales in 1983 and of Scotland in 1989
(3).
During the first half of the 20th century a greater understanding of soil chemistry and plant
nutrition provided the impetus both to establish the extent of variation in agricultural soils through
soil survey and to gain greater understanding of how to mange their nutrient status to support a variety
of crops. This was a period during which the Agricultural Research Council was established (1934) and
the Departments of Agriculture began to take initiatives during and after World War II to improve output
from British agriculture. Thus the funding for soil science during this period was predominantly from
the public purse. The rapid development of soil science and the need to increase crop yields were
primary drivers during this period.
From 1975
These drivers continued to influence developments into the third quarter of the 20th century.
In parallel with the other sciences supporting agriculture there was a rapid growth in funding for soil
science and in technological development to produce the bulk of our ‘food from our own resources’. This
was the case not only in the UK but also in the USA. Commenting on this period, Warkentin (1992),
states ‘Crop production was the engine driving this effort, and its emphasis was on inputs rather than
on managing systems. …..During this period there was little emphasis on reasoning from processes, it was
considered better to measure effect even if it were over short time periods.’
Excellent empirical solutions to problems came out of this effort. For example, answers to how much
N fertiliser should be added for maximum crop production were sought and given. There was, therefore,
little information developed on the underlying processes or on phenomena that had time scales of more
than one or two years. This seems to have delayed an interest in and understanding of the biological
processes in soils (4). Much of the research of this period was classified as being applied
and descriptive. Nevertheless, through the application of more sophisticated soil analysis techniques
and the use of soil survey data to produce land capability and suitability maps, soil technology and the
results of ‘fertiliser dose-response’ experiments provided the basis for increasing crop yields
significantly during this period.
Then, following first the Rothschild Report in 1971, which embodied the customer-contractor principle
but which was critical of the Agricultural Research Council and second, the report of the Advisory
Committee for Applied Research and Development in 1975, which emphasised the relevance of public
research to manufacturing and industry, funding for agricultural research was reduced. Consequently
Agricultural Departments and the ARC began a process of prioritisation and a reduction in the numbers of
scientists involved in agricultural research.
By the early to mid 1980’s this process had gathered pace: furthermore the increased output from
agriculture and the oversupply of agricultural commodities within Europe brought into question the
continued public investment in agricultural research. This was considered also in relation to the need
for public research investment to support other industries and the need to improve their competitiveness.
The lack of private and commercial investment in agricultural research also began to influence funding
policy. Moreover, in 1984 ARC became AFRC, the Agricultural and Food Research Council, with
responsibility to include research to address concerns about food safety. Funding for agricultural
research continued to be redeployed.
.The negative impact on agricultural soil science research funding in the UK over this period was
considerable. During the process of prioritisation several factors appear to have influenced the
reduction in resources allocated to soil science. The large increases in crop yields that had been
achieved were the result of many improvements in technology – crop breeding, methods of disease and weed
control, and not least the information that related crop yield to fertiliser inputs for different soil
types and cultivation regimes. With regard to the latter soil science was deemed to have delivered.
In addition, government policy development indicated that it wished to remove funding from ‘near market
research’ such as this, which it did eventually in 1990.
Priorities were also determined by judgments about the potential for innovation within different
areas of science supporting agriculture and the growth of agribusinesses. Developments in cell and
molecular biology, and plant genomics were judged to show real promise: with its responsibility to fund
science that had the potential to underpin future commercial developments the AFRC moved greater
resources into this area of biotechnology. By the mid 80’s agricultural soil science seems to have
reached a plateau in terms of development and lost some of its innovative zeal. Its period of empirical
research appears to have been judged at this time to have been too applied and too ‘near market:
therefore, in the ‘cut and thrust’ of prioritisation soil science ‘lost out’.
1990 onwards
A combination of several changes in research policy direction and an unfavourable view of the
current innovative status of soil science at the time led to a greatly reduced capacity for agricultural
soil science in the UK by the beginning of the 1990’s. While the principle driver for soil science up
to the mid 80’s had been to improve crop yields, this was no longer a priority in terms of government
research funding for the rest of the century. In terms of attracting funding agricultural soil science
had lost its appeal.
However, a core capability was sustained and soil biologists were already contributing to approaches
that moved the emphasis towards process based research and mathematical modelling. Modelling provided
the impetus to gain a much clearer and quantitative understanding of nutrient cycling, particularly
nitrogen and carbon. It also led to an interest in processes at the scale of the rhizosphere.
Developments in microbiology have led to a greater ability to identify the role of populations of
microbes in nutrient cycling and how specific organisms can be used to identify the resilience of soils
to pollutant damage as well as being used as toxic indicators in water.
The early 90’s was a period of refocus for soil science in the UK. It became apparent that the
issues of public concern were the impact of acid rain and fertilisers on water quality and the ecology
of rivers, and the resilience of soils to the impact of waste, and heavy metals as pollutants. There was
a decisive shift towards a broader interest in the role of soils in the environment and ecosystem
function. As a corollary soil research for agriculture became concerned with the more efficient use of
fertilisers and effective use of farmyard manures, and a small amount of research to support the
development of organic farming. These were the issues that became the primary drivers during much of
the 90’s for the limited amount of soil research that was funded.
At an international level an important impetus developed in the late 90’s prior to and following the
Kyoto Protocol to the UN Framework Convention on Climate Change which was signed in December 1997. The
Protocol contains legally binding commitments to limit or reduce greenhouse gas emissions within the
period 2008-2012 by at least 5% below 1990 levels. Europe’s commitment is to achieve an 8% reduction
and the UK has committed itself to a 12% cut with a voluntary target of 20% below that of 1990. However,
associated changes in the net fluxes of two other greenhouse gases identified in the Protocol – nitrous
oxide and methane – will have to be taken into account. The problem of how to quantify the soil sources
and sinks, to maximise carbon sequestration, and to minimise soil emissions of methane and nitrous oxide
presents a major scientific challenge to the soil science community over the next few years,
(Smith, 1999) (5).
The European Commission has concluded that the management of our soil resource is central to
environmental ecosystem sustainability; it requires to be managed, to be conserved and protected.
This has led to the proposal to have a soil monitoring directive and the establishment of criteria of
soil quality. Research in some countries of Europe including the UK has been stimulated in anticipation
of having to implement these proposals.
A recent UK Soil Research Audit, commissioned by Defra as part of its Soil Action Plan for England
2004-06, concluded that now was a time of great opportunity and challenge for soil research because an
increased knowledge base allowed some of the major environmental issues to be tackled, including climate
change, pollution and sustainable land management.
Directions for the 21st Century?
Many now argue that biology lies at the heart of the scientific enterprise of the 21st century but
also see soil science as an integral part of that enterprise. Important practical issues require soil
biology knowledge. These include understanding the role of soil processes in global warming and
strategies to ameliorate it; enhanced and safe recycling of waste from manures, urban and industrial
activity; pollutant destruction at waste disposal sites as well as landscapes contaminated from natural
processes; biological control of rhizosphere pests; enhanced groundwater quality; discovery of new
biotechnological products, including pharmaceuticals, pesticides and enzymes from the undiscovered
microbial diversity of soil; and optimising recycling of soil nutrients for sustainable agriculture and
forestry, Tiedje, (2001) (6). The basic premise behind an attempt to understand the complex
soil community is that further knowledge will pay off in improved agriculture, environmental
decision-making and management, and many of the practical issues listed above.
Where do we go from here?
Questions:
So where are we now? What are the current drivers for soil science in the UK? Are they explicit?
Does our programme of soil science research reflect the issues that are of concern to the
stakeholders and the public in so far as these can be defined? Are farmers’ concerns being addressed?
Was the redirection of resources away from agricultural soil science in the 1980a appropriate in the
limited funding environment of the time, given the plateau in its development and the promise of other
areas? Has this had any negative consequences? Is there still a benefit to be gained from traditional
agricultural soil science and is more needed?
(1) - This paragraph is based on the first chapter of 'History of Soil Science': an international perspective/Dan H.Yaalon, and S.Berkowicz (ed.). Reiskirchen: Catena Verl., 1997: Advances in Geology 29 (2) - Greenland D.J. (1997) Inaugral Russel Memorial Lecture - Soil Conditions and Plant Growth, Soil Use and Management 13, 169-177 (3) - Hollis, J M and Avery, B W (1997) History of Soil Survey and Development of the Soil Series Concept in the UK, Advances in Geology 29 (4) - Warkentin, B P (1992) 'Soil Science for Environmental Quality - How do we know what we know?' J. Environ. Qual. 21 163-166 (5) - Smith, K A (1999) After the Kyoto Protocol: Can soil scientists make a useful contribution? Soil Use and Management 15 71-75 (6) - Tiedje, J M, Cho, J C, Murray, A, Treves, D, Xia, B & Zhou (2001) Soil Teeming with Life: New Frontiers for Soil Science in Sustainable Management of Soil Organic Matter eds RM Rees, B C Ball,
C D Campbell and C A Watson