Life in extraordinary concentrations (a tribute to Peter Beuge)
© Matschullat; licensee Springer. 2012
Received: 13 June 2012
Accepted: 29 June 2012
Published: 3 October 2012
Our growing humankind needs fertile soils for its sustainable development. Population growth and related use of resources, jointly with environmental pollution seem to contradict that demand. Recently available geochemical atlases allow for a better assessment of representative soil chemistry and potential pollution status, and thus for more efficient planning and development.
Despite millennia of human soil use (agriculture and forestry) and perceived abuse (mining etc.), most of Europe’s soils are on the continental scale more strongly influenced by natural forces (primarily geology/lithology) than by human impact. Even in large conurbations (e.g., Berlin), baseline values can be encountered in the city centre and in spatial proximity to highly contaminated sites. In a country like Brazil, where significant human impact started only about 500 years ago, challenges appear more demanding, due to the very old age of most soils and a radical depletion of nutrients. Yet, relatively recent site-specific to local contamination appears almost negligible in comparison, again corroborating the dominant role of natural forces and processes (geology, climate). Both regions, representing significant northern and southern hemispheric conditions, show for most chemical elements a very wide natural concentration range.
The objective necessity to clean up polluted sites and to avoid additional soil pollution can be strongly supported by acknowledging the highly localized true contamination of soils. Related governmental regulations (threshold values etc.) should be applied with a deeper understanding for natural variability and for real risks involved in positive pedogeochemical anomalies, thus saving money and frustration.
KeywordsPedogeochemistry Threshold values Background or baseline values Europe Brazil Australia
Soil protection is one of the global challenges to be met by the growing humankind. The topic is partly directly related to further world population growth; at least to the mid 21st Century, when 9 billion people are expected to populate the planet. The term “soil protection”, in analogy to “species protection, water and climate protection” already suggests that this basic life-sustaining resource is under pressure. The book “Dirt” by, vividly illustrates these pressures, their causes and historical development, and shows pathways to solutions. Yet, major misperceptions persist not only amongst laypeople, when it comes to soil pollution issues. Various places exist – the county of Freiberg, Saxony, Germany, is one of them – where centuries of metal mining and smelting history have left a legacy that, seen through the eyes of regulators, are not fit for sustaining healthy human life. That motivates the title of this contribution, which is a quote from my deceased colleague and predecessor Peter Beuge, professor of Geochemistry at TU Bergakademie Freiberg, who contributed significantly to the topic.
A widespread perception sees a detrimental large-scale contamination of soils, particularly in industrial countries. This paper compares two regions of almost similar size, representing the northern hemisphere and partly dense industrial legacy (Europe) and the southern hemisphere with limited industrial history (Brazil, and some data from Australia). This contribution focuses on inorganic components. Yet, the key hypotheses are conferrable to organics – with the major difference that the latter show partly much shorter soil retention times due to metabolic decay.
The following two key hypotheses are being discussed:
Relevant (for ecosystems, human health), human triggered soil contamination does not occur ubiquitously, but is largely highly locally focused (Table1; Figures1 and2) – an important starting point for constructive solutions,
The soil chemistry of Europe as an example for the mostly temperate humid climate zone is distinctively different from those in (sub)tropical regions (e.g., Brazil).
Recommended nomenclature for spatial scales
50—500 Mio. km2
5—50 Mio km2
0.5—5 Mio km2
50,000 m2 – 0.5 km2
5,000 – 50,000 m2
500 – 5,000 m2
50 – 500 m2
5 – 50 m2
0.5 – 5 m2
500 cm2 – 0.5 m2
50 – 500 cm2
5 cm2 – 50 cm2
Concentration ranges of selected trace elements from European soils and surface waters (total concentrations from) and in ground waters (Reimann and Birke 2010; *here 95 percentile)
Results and discussion
To its eastern boundary at the Ural mountains, the continent represents an area of ca. 10.18 million km2 and houses a currently slightly declining population of about 740 million (2011) with a density of 76 people per square kilometre. Climatologically, the spectrum reaches from the subarctic (low population density) to the Mediterranean space (higher population density) with an emphasis on the temperate humid climate (highest population density). Various cambisols and podsols dominate the soil types. The land-use is defined by forestry (ca. 40%) and agriculture (ca. 40%), with strong sub-regional heterogeneities (e.g., agriculture 2.2% on the Faroe Islands to 75.6% in Moldavia; Worldbank). Population density and its consequences on land-use increased in various steps since the Bronze Age; 4,000 years ago. Today, the human population stagnates and is sub-regionally slightly decreasing. Locally highly restricted “hot spots” of soil and sediment contamination evolved as of the Bronze Age, visible even on continental scale geochemical maps. Almadén (Spain), Goslar (Germany) and SW-Wales (Great Britain) may serve as related examples; partly noticeable in Figure1. Source for each of these anomalies are rich mineralisations with local mining and smelting activities. Even without the human activities, positive anomalies would be detectable – albeit even more spatially focussed; mining and smelting have often contributed to a higher spread and to increased surface concentrations.
The official (proven) history of mining in the Erzgebirge [ore mountains] began in Carolingian times (9th Century AD;[6, 7]). Latest starting in the 12th Century, extensive base metal, tin and silver deposits led to a fast regional development that persisted with various interruptions into the 20th Century. Today, and due to the global market prices and the demand for metallic resources, another renaissance emerges[8, 9]. Centuries of mining and smelting activities, mostly without any environmental protection technologies, as we know them today, led to a radical alteration of (sub-) local pedogeochemistry with anomalies that may exceed local geogenic background values by several orders of magnitude. For a long time, the city of Freiberg was referred to in popular parlance as ABC-city: in short for the complex soil pollution with arsenic (A), lead (Pb = B) and cadmium (C); see Figure2.
This contamination is not area-representative, however – neither for Saxony and Germany, nor for Europe. The contamination must not even be dangerous or threatening – here, the chemical (and mineral) bond of the potentially toxic elements defines the risks involved. It is critical whether the dispersion of the positive anomaly leads to an increased bioavailability that permits a toxicologically relevant input of toxins within relatively short time increments (fluxes) into the food chain or surface waters and groundwaters, or the risk of direct skin contact and geophagy. The dominant climatological conditions with still more or less regularly distributed annual precipitation and a closed vegetation cover for much of the year additionally slow down the mobility and dispersion of potentially toxic compounds. A closer look as soil geochemical data demonstrates that geological forces shape the concentrations and occurrence patterns of the elements – even in densely populated (e.g., Berlin) and highly industrialised Central Europe. In large cities such as Berlin, there are certainly (and partly relevant) human-induced positive anomalies. At the same time, background values do occur even in the inner city environment and they dominate the city perimeter. The hypothesis is that the distribution patterns of European soil chemistry – at least when investigated on a continental scale – is dominated by the Quaternary glacial history in the northern half of Europe, and even Tertiary processes in its southern half[11–14]. Such influence of the Quaternary climate history (and partly older) with its coupled geological and pedological consequences is equally applicable to vast areas of the northern hemisphere, mainly Russia, the northern part of the USA and Canada.
The country has continental dimensions with its area of 8.51 Mio. km2. The current population number amounts to about 192 million (2011) with a density of 22 people per square kilometre. Most of the country is subject to tropical, in its south partly subtropical conditions. Different from Europe, these climates prevailed also during the Quaternary. Oxisols and ferralsols as well as podsols dominate the country’s soil cover. Its land-use has experienced radical changes as of post-Columbian times; the last 512 years. Agricultural production prevails over ca. 31% of the area, near natural forest covers about 27% of the country; the total forested area amounts to 55% (Worldbank). The rather small share in agricultural land-use is explained by the large share of the semi-arid Caatinga biome in the Northeast with dominating extensive agriculture (mainly cattle ranching). Nevertheless, livestock farming is responsible for decreasing forest area in originally pristine forests in the neighbouring Cerrado biome.
Median values and ranges (except for WSA) of major, minor (wt-%) and selected trace elements (mg kg -1 ) in surface mineral soils: World Soil Average (WSA), BraSol 2010, NGSA, FOREGS*
Ba (mg kg-1)
Ce (mg kg-1)
Cr (mg kg-1)
Cu (mg kg-1)
Mn (mg kg-1)
279 (0.5 – 3,740) #
P (mg kg-1)
Pb (mg kg-1)
Rb (mg kg-1)
S (mg kg-1)
Sr (mg kg-1)
Ti (mg kg-1)
V (mg kg-1)
Zn (mg kg-1)
Zr (mg kg-1)
This change that encompasses the development of industrial agriculture, takes place on soils that are partly several tens of millions of years old. Soils that – different from those in Europe and North America have left behind their state of maturity and which are partly decoupled from their bedrock lithogeochemistry[11, 19, 20].
The biomes have adapted in an evolutionary manner to regional element cycles and carry voluptuous vegetation wherever enough water is available – despite very low nutrient availability. Yet this constellation challenges the modern agricultural practice and human adaptive capacities if sustainable land-use is to be achieved despite the unfavourable boundary conditions (nutrient, humus). This challenge appears much more demanding than the often-negative consequences of locally intense mining and ore processing activities that leaves, similar to North America and Europe a strictly local “footprint” – with problems analogue to those described above.
The term „soil protection” is per se rather imprecise – similar to the terms species protection, water protection and climate protection. To develop an appropriate and sustainable soil protection (strategy), an initial and thorough investigation of the soil status is needed, including the explanation why the current status is the way it is and which processes were and are responsible. This is true for any spatial scale; yet a local or even spot analysis may require modified methods as compared to a regional or continental approach. Neither of these points is currently common practice, as numerous examples have shown, including the North American and European forest decline story of the 1970’s and 1980’s. The required knowledge is a non-negotiable base for any type of measure to improve or preserve e.g., soil fertility, or to allow for a desired land-use over extended periods of time (human generations). Depending of the defined goals and the objective necessities, consequences and boundary conditions emerge that allow the decision makers to trigger meaningful measures and activities.
Starting with the initially formulated hypothesis, the given examples (and many others) demonstrate that anthropogenic soil pollution does not occur ubiquitously and that even in densely populated areas (e.g., Berlin) such pollution may be negligible on a sub-local level (e.g., large individual property, city block). Such insight eases the distinct identification of truly contaminated areas that may then be treated appropriately. Such action may reach from rather inexpensive withdrawal from common use to partly very expensive remediation. Soils of different climate zones and regions significantly differ in their geochemistry (and their ages and thus their history). Thus simplifying global average values (such as WSA) is of limited if any value or even misleading for almost any concrete situation. This is similarly true for the uncritical and un-adapted use of threshold or limit values and related environmental standards. Their application appears meaningful under the fulfilment of three boundary conditions only: i) the values are adapted to a defined space, for which the respective directive or law has been formulated; ii) the values will include the potential and real mobility of the related elements and thus their bioavailability (binding forms, redox and pH-conditions); and iii) the values will not be statistically defined for larger areas (see i), but are exclusively based on toxicological evidence. The latter presents a major challenge and effort, yet it should, e.g., applied to a country like Germany, demand in total a lot of superfluous work and costs, and will thus permit much more targeted and efficient solutions.
Peter Beuge was a full professor for Geochemistry at the Institute of Mineralogy at TU Bergakademie Freiberg. He died prematurely, fighting a terminal cancer. The title stems from his words. He always tried to go “behind the scenes” of any issue and to pose the truly relevant questions instead of the “politically correct” ones. Thanks go to Alexander Pleßow, Clemens Reimann and Eleonora Deschamps for their critical comments to a previous version of this paper, to Gerald Schmidt for opening the door to this journal and to various colleagues from the International Geochemical Mapping Programme, whose most constructive criticism and valuable suggestions over the years have certainly influenced my own thinking.
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