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Misconception Number 13: In tropical countries, the limiting factor for soil fertility is phosphorus, which cannot be recovered through atmospheric fixation with leguminous plants, as is possible for nitrogen. In areas where there is no natural reserve of phosphorus available, Organic Agriculture cannot work because the only way to maintain soil fertility is to bring in synthetic P fertilizers.
Summary of Counter-Arguments:
- Organic farms usually implement a range of practices that increase phosphorus inputs and phosphorus recycling and reduce phosphorus losses at the farm level. - Synthetic P fertilizers are made from rock phosphates that are chemically modified. Organic Agriculture allows the use rock phosphates (PRs) that are only physically (mechanically) modified. They are less energy intensive, more affordable, better for building the soil’s long term fertility and as easily transportable as the chemically modified phosphorus.
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Details of Counter-Arguments:
The question of replenishment of phosphorus
levels in tropical organic agricultural systems is indeed seen by many
agronomists as one of the main challenges for the long-term productivity
of organic farms. The problem is assumed to be more serious in Sub-Saharan
Africa because the soluble content of phosphorus on bedrock is quite low
in many regions. However, many field observations suggest that the phosphorus “nutrient cycle problem” is
not more difficult to solve in Organic Agriculture than in conventional
agriculture.
When
considering Organic Agriculture at the farm level, there are several
possible inflows of phosphorus. Organic inputs can be brought from
outside the farm (e.g., through grazing, collection of wild products, and organic
amendments such as peat, guano, and seaweeds). Agro-forestry practices can
also increase the nutrient take-up from the subsoil through the deep-penetrating
roots of trees (and other perennial crops).
Organic standards permit
the use of clay and rock phosphates (PR), both of which containing
phosphorus. Although the use of
rock phosphates is not currently common in tropical countries, and in
Africa in particular, there is considerable potential for improvement in
extraction methods and also regarding transport and distribution to
farmers that would assist countries in Africa and tropical countries
outside of Africa in the use of rock phosphates. There are substantial
deposits in various countries across Africa and some of these countries,
such as Togo, Senegal, Morocco,
and Tunisia,
even export to the world market. In addition, many rock phosphate deposits located in the tropics and subtropics are
still un-tapped. [1]
Countries like Mali
and Burkina Faso
have deposits that they want to develop for local markets, with the
intention of increasing the use of rock phosphate and replacing imported
fertilizers. Further anticipated developments, including improvements in
economies of scale, and logistics, more and more farmers will have access to
natural phosphates when needed. Technically, there is no reason why the
transportation cost of natural phosphate (per unit of P) should be higher
than the transportation cost of synthetic phosphate. Indeed, rock
phosphate has a concentration between 32 and 35 percent p205, which is
comparable to the concentration of synthetic phosphorus fertilizers (most
traded superphosphates average 36 percent p205, while single
superphosphate is sold in some markets with a p205 content of around 18 percent).
Except for some
nitrogen-based fertilizers, almost all conventional, chemically processed
‘industrial’ fertilizers are chemically processed rocks. Synthetic P
fertilizers are derived from rock phosphates that have been chemically
modified. In contrast, agrominerals used in Organic Agriculture are
commonly only physically modified, by crushing and grinding. [2] The production of rock phosphate
relies on the same raw materials as production of chemically processed P
fertilizers, but is less energy intensive. Superphosphates have high energy cost components and are
already too expensive to be affordable in adequate amounts by low output
farmers–unless continuous subsidies are provided by taxpayers or donors. The
difference is that, in most conditions, phosphorus from rock phosphate is
not as immediately available to plants as superphosphate (which is water soluble
by treatment with acid); it is broken down into forms available to plants
over a longer period (e.g., five years). It is nevertheless possible to
use several biological means to increase the availability of P from rock
phosphate in the first years (e.g., phospho-composting, inoculation with vesicular-arbuscular
mycorrhizal fungi, use of phosphate solubilizing
micro-organisms that enhance PR dissolution and P availability to plants).
Many leguminous plants (which are commonly used in typical organic
rotations) also facilitate the solubilization of rock phosphate. Moreover,
by reducing Ca activity in the soil solution, the presence of organic
matter (Ca-sink) in the soil helps to quicken the dissolution of PR.
Hence, the impact of PR application will be realized more quickly in a
well-managed organic field. However, organic is a long term project [3].
Organic practitioners understand that building healthy and truly fertile
soil takes time, which is one of the reasons they employ techniques that
work over longer periods of time than the growing season. Bringing readily
soluble, synthetic fertilizers to the soil will only provide from one to
three nutrients for the current growing season, but will undermine the
broader fertility of the soil in the mid to long-term. On the contrary,
rock phosphates and other natural mineral fertilizers commonly have
long-term residual effects and contribute to recapitalization of nutrients
in the soils.
The current loss of phosphorus observed in
Africa, also has a lot to do with the fact that a large percentage of Africa’s food producing areas consists of farming
characterized by very small family farms that have very little access to
any kind of inputs (synthetic and natural P fertilizers alike). This means
that alternative ways of improving the nutrient balance have to be developed
and implemented, and that reducing nutrient losses on the farm will play a
major role. Organic Agriculture can
significantly reduce the outflow of phosphorus from the farm through
recycling of crop residues and animal wastes and because it results in higher
organic matter content in the soil, which helps reducing erosion and
nutrient run off and increases the soil’s cation exchange capacity (CEC).
Phosphorus consumed by both humans and animals is rejected through their
waste. Too often, nutrients contained in these wastes end up getting
flushed into waterways, disturbing their ecosystem and ultimately causing
water pollution and insalubrity problems. Recycling animal wastes
(including bonemeal, chicken manure and bat droppings) and human wastes
through on-farm composting and, perhaps, ecological waste (water and
solid) management systems could help significantly reduce the phosphorus
losses.
While studies of soil fertility at the national
level in Africa present negative nutrient
balances (even under conventional agriculture), the picture is more varied
at field and farm levels where households have developed a wide range of
management strategies [4]. It is often hard to
quantify the effect of organic management practices on nutrient cycles because of the fact that Organic Agriculture isn't about
like-for-like input substitution, but rather the overall development of
healthy soil. Unlike synthetic fertilizers, organic fertilizers often
have a complex and variable nutrient composition, which makes the
collection of data a much more complex enterprise. A related problem is
the lack of research on organic and natural mineral fertilizers (e.g.,
less research tends to be done on rock phosphate than on synthetic P
fertilizers since fertilizer manufacturers have an economic interest in
selling superphosphates). Agricultural research institutes and extension
services are also still convinced that chemically-processed fertilizers
are indispensable.
Let’s also not forget that, although low soil fertility is one cause of Africa’s
food insecurity, it is certainly not the only cause. Social and
economic determinants are at least as important. There is increasing
evidence that it is not only supply factors, such as productivity per
hectare, but rather demand factors, such as market opportunities and
access, that determine agricultural development outcomes in Africa. Organic agriculture, by offering new and
rewarding market opportunities for African smallholders, can help rural
families find a way out of poverty, and can provide them with the
incentive to invest in enhancing the soil fertility of their land holdings.
[1] Use of Phosphate Rocks for Sustainable Agriculture (FAO, 2004) http://www.fao.org/docrep/007/y5053e/y5053e00.htm
[2] The reader may want to check on the excellent book written by Peter van Straaten: Rocks for crops, available online at http://www.uoguelph.ca/~geology/rocks_for_crops/
[3] This is addressed in the IFOAM Basic Standards, which state that “Mineral fertilizers shall only be used in a program addressing long-term fertility needs..”.
[4] Nutrients on the Move: Soil fertility dynamics in African farming systems, Thea Hilhorst and Fred Muchena (2000).
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