Restoring Soil Quality to Mitigate Soil Degradation

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Restoring Soil Quality to Mitigate Soil Degradation

Transcript Of Restoring Soil Quality to Mitigate Soil Degradation

Sustainability 2015, 7, 5875-5895; doi:10.3390/su7055875 Article

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sustainability
ISSN 2071-1050 www.mdpi.com/journal/sustainability

Restoring Soil Quality to Mitigate Soil Degradation

Rattan Lal

The Ohio State University, Columbus, OH 43210, USA; E-Mail: [email protected]; Tel.: +1-614-292-9069

Academic Editor: Marc A. Rosen

Received: 31 March 2015 / Accepted: 5 May 2015 / Published: 13 May 2015

Abstract: Feeding the world population, 7.3 billion in 2015 and projected to increase to 9.5 billion by 2050, necessitates an increase in agricultural production of ~70% between 2005 and 2050. Soil degradation, characterized by decline in quality and decrease in ecosystem goods and services, is a major constraint to achieving the required increase in agricultural production. Soil is a non-renewable resource on human time scales with its vulnerability to degradation depending on complex interactions between processes, factors and causes occurring at a range of spatial and temporal scales. Among the major soil degradation processes are accelerated erosion, depletion of the soil organic carbon (SOC) pool and loss in biodiversity, loss of soil fertility and elemental imbalance, acidification and salinization. Soil degradation trends can be reversed by conversion to a restorative land use and adoption of recommended management practices. The strategy is to minimize soil erosion, create positive SOC and N budgets, enhance activity and species diversity of soil biota (micro, meso, and macro), and improve structural stability and pore geometry. Improving soil quality (i.e., increasing SOC pool, improving soil structure, enhancing soil fertility) can reduce risks of soil degradation (physical, chemical, biological and ecological) while improving the environment. Increasing the SOC pool to above the critical level (10 to 15 g/kg) is essential to set-in-motion the restorative trends. Site-specific techniques of restoring soil quality include conservation agriculture, integrated nutrient management, continuous vegetative cover such as residue mulch and cover cropping, and controlled grazing at appropriate stocking rates. The strategy is to produce “more from less” by reducing losses and increasing soil, water, and nutrient use efficiency.
Keywords: soil resilience; climate change; soil functions; desertification; soil carbon sequestration

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1. Introduction
Of the 5.5 billion people living in developing countries in 2014 [1], a large proportion of them depend on agriculture for their livelihood. In fact, one billion of these people are small landholders who cultivate <2 ha of land [2]. With limited resources and poor access to inputs, management of soil quality is essential to strengthen and sustain ecosystem services. Soil degradation is a 21st century global problem that is especially severe in the tropics and sub-tropics. Some estimates indicate degradation decreased soil ecosystem services by 60% between 1950 and 2010 [3]. Accelerated soil degradation has reportedly affected as much as 500 million hectare (Mha) in the tropics [4], and globally 33% of earth’s land surface is affected by some type of soil degradation [5]. In addition to negatively impacting agronomic production, soil degradation can also dampen economic growth, especially in countries where agriculture is the engine for economic development [6]. Over and above the environmental and economic impacts, there are also health risks of soil erosion [7] and other degradation processes [8].

Figure 1. Types of soil degradation.
Soil degradation implies a decline in soil quality [8] with an attendant reduction in ecosystem functions and services. Conceptually, there are four types of soil degradation: (i) physical; (ii) chemical; (iii) biological; and (iv) ecological (Figure 1). Soil physical degradation generally results in a reduction in structural attributes including pore geometry and continuity, thus aggravating a soil’s susceptibility to crusting, compaction, reduced water infiltration, increased surface runoff, wind and water erosion, greater soil temperature fluctuations, and an increased propensity for desertification.

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Soil chemical degradation is characterized by acidification, salinization, nutrient depletion, reduced cation exchange capacity (CEC), increased Al or Mn toxicities, Ca or Mg deficiencies, leaching of NO3-N or other essential plant nutrients, or contamination by industrial wastes or by-products. Soil biological degradation reflects depletion of the soil organic carbon (SOC) pool, loss in soil biodiversity, a reduction in soil C sink capacity, and increased greenhouse gas (GHG) emissions from soil into the atmosphere. One of the most severe consequences of soil biological degradation is that soil becomes a net source of GHG emissions (i.e., CO2 and CH4) rather than a sink. Ecological degradation reflects a combination of other three, and leads to disruption in ecosystem functions such as elemental cycling, water infiltration and purification, perturbations of the hydrological cycle, and a decline in net biome productivity. The overall decline in soil quality, both by natural and anthropogenic factors, has strong positive feedbacks leading to a decline in ecosystem services and reduction in nature conservancy. Once the process of soil degradation is set-in-motion, often by land misuse and soil mismanagement along with the extractive farming, it feeds on itself in an everincreasing downward spiral (Figure 2).

Figure 2. The downward spiral of decline in soil and environment quality exacerbated by indiscriminate plowing, residue removal and extractive farming.

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The objectives of this review are to: (1) deliberate the role of soil resources in provisioning essential ecosystem services; (2) illustrate the impacts of soil degradation on decline in ecosystem services; and (3) identify strategies for improving soil quality to mitigate risks of soil degradation.
2. Soil and Ecosystem Services
Soil, the most basic of all resources, is the essence of all terrestrial life and a cultural heritage [9]. Yet, soil is finite in extent, prone to degradation by natural and anthropogenic factors, and is non-renewable over the human timescale (decades). Soil quality also has strong implications to human health [8,10], thus illustrating its important role in both society and the environment. Because of numerous ecosystem services provisioned through soils (e.g., food, feed, fiber, climate moderation through C cycling, waste disposal, water filtration and purification, elemental cycling) [11,12], soil quality must be protected or restored to enhance these services. Increased public awareness and a fundamental understanding of basic pedospheric processes (i.e., biology, chemistry, physics, pedology, ecology) are essential both to enhancing long-term productivity and improving the environment [13].
3. Soil Organic Carbon and Its Impact on Soil Quality
The SOC pool, including its quantity and quality, is the defining constituent of soil [14,15]. Indeed, SOC pool is the most reliable indicator of monitoring soil degradation, especially that caused by accelerated erosion [16]. Soil degradation depletes the SOC pool, along with it, plant available N and other essential nutrients such as P and S. Furthermore, as identified repeatedly in this special issue of Sustainability, depletion of SOC pool is a global issue and a principal cause of soil degradation, especially in the European semi-arid Mediterranean regions [17]. Developing strategies to ensure the SOC pool is to increase and preferably maintain above the threshold or critical level of 10 to 15 g/kg (1.0%–1.5%), which is essential for reducing soil degradation risks and reversing degradation trends. Integrated nutrient management (INM) is one strategy that embodies sustainable management of the SOC pool and its dynamics [18]. Adoption of INM or similar management practices that create a positive soil/ecosystem C budget can not only increase productivity but also sequester additional atmospheric CO2 into the SOC pool. This has been documented for many surface soils within the U.S. Corn Belt which act as C sinks when corn (Zea mays L.) is grown using recommended management practices (RMPs) such as conservation agriculture (CA) [19]. There also exists a strong relationship between vegetation cover and the SOC pool, such that excessive reductions in vegetation cover exacerbates risks of soil degradation and SOC depletion. A study conducted in the sub-tropical humid grasslands in South Africa indicated that the decline in grass (vegetative) cover from 100% to 0%–5% reduced the SOC pool by 1.25 kg/m2 and the soil organic N (SON) pool by 0.074 kg/m2 [20], There were also attendant declines in the C:N ratio and proportion of SOC and SON in the silt + clay fraction with the decline in aerial grass cover which negatively affected ecosystem functions of the acidic sandy loam soils. Similarly, transformation of a thicket vegetation to an open savanna (dominated by grasses) due to intensive grazing decreased soil quality in the Eastern Cape region of South Africa [21]. Indeed, savanna soils have lower SOC concentration and a greater tendency to crust than thicket soils because of the decreased quantity and stability of structural aggregates.

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The widespread prevalence of degraded soils in sub-Saharan Africa (SSA), a classic example of a downward spiral, is attributed to over exploitation, extractive farming, low external inputs, and poor or improper management (Figure 2). Accelerated degradation is shrinking the finite soil resource even more rapidly in these regions of harsh climate and fragile soils. In this context, enhancing the SOC pool is important to sustain soil fertility and agronomic productivity [22]. Simply adding chemical fertilizers or improved varieties, as is often erroneously recommended even by well-intended advocates, is not enough.
The SOC pool of agricultural soils of West Africa, similar to those of croplands in other developing counties (e.g., South Asia), is severely depleted by over-exploitation of natural resources [23]. These soils must therefore be managed to increase both soil C and vegetation [24,25] to restore the degraded agroecosystem services. Changes in aerial vegetative cover could thus be used as an early indicator of shifts in soil ecosystem functions within fragile environments. A shift in vegetative cover may be caused by alterations in land use or climate change. In addition to SOC and SON pools, soil moisture regime is another important indicator of climate change [26]. In conjunction with changes in soil moisture regimes, projected global warming may also influence SOC decomposition rates [27,28] including that of fine woody debris. Field experiments have shown that warming increases mass loss for all vegetative species and size classes by as much as 30%. However, larger debris and that with higher initial lignin content decomposes more slowly than smaller debris and that with lower antecedent lignin content. Indeed, degradation of lignin may not follow the same trend as that of total mass loss [29]. Along with the adverse effects of soil erosion and other degradation processes, the SOC pool is also prone to climate change and associated alterations in temperature and moisture regimes.

Figure 3. The process-factor-cause nexus as a driver of soil degradation.

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The self-reinforcing soil degradation process (Figure 2) is strongly exacerbated by the interaction between processes, factors and causes of soil degradation (Figure 3). Processes include the mechanisms (types) of soil degradation. Factors comprise agents of degradation related to natural or anthropogenic drivers such as climate, physiography, socio-economic or ethnic/cultural parameters. Causes of soil degradation include specific activities which aggravate the adverse effects of processes and factors. Examples of specific causes include activities such as deforestation, land use conversion, extractive farming practices or over-exploitation, excessive grazing, excessive plowing etc. (Figure 3). The process-factor- cause nexus is strongly impacted by site-specific conditions. Thus, understanding the nexus or connectivity is critical to restoring soil quality and mitigating degradation.
4. Soil Quality Index
The SOC pool is a key indicator of soil quality, and an important driver of agricultural sustainability. In addition to its amount, other parameters of SOC include its depth distribution, quality or attributes (physical, chemical, biological), and the turnover rate or the mean residence time (MRT). Relevant indicators of soil physical quality include amount and stability of aggregates; susceptibility to crusting and compaction; porosity comprising of pore geometry and continuity; water transmission (infiltration rate and amount) and retention as plant-available water capacity (PAWC); aeration and gaseous exchange; effective rooting depth; soil heat capacity and the temperature regime. Similarly, appropriate indicators of soil chemical quality include pH, CEC, nutrient availability; and favorable elemental balance and lack of any toxicity or deficiency. Relevant indicators of soil biological quality are microbial biomass C (MBC), activity and diversity of soil fauna and flora, absence of pathogens and pests as indicated by a soil’s disease-suppressive attributes. An optimal combination of these properties affects agronomic productivity; use efficiency of water, nutrients and other inputs; and sustainability of management systems. Indicators of soil quality differ among soil types, climates and land uses. For example, there are specific soil quality indicators for the intensively managed soils of the Indo-Gangetic Plains [30] that will differ from those for tropical Alfisols in semi-arid regions [31–34]. A spectral soil quality index based on application of reflectance spectroscopy has also been proposed as a diagnostic tool to assess soil quality [35]. This technique can provide a characterization of physical, chemical and biological attributes that can be merged together to indicate how well a soil is functioning for a specific use [36–39].
5. Conservation Agriculture and Soil Quality
Four basic principles of CA are [40]: (i) retention of crop residue mulch; (ii) incorporation of a cover crop in the rotation cycle; (iii) use of INM involving combination of chemical and bio fertilizers; and (iv) elimination of soil mechanical disturbances. Properly implemented on suitable soil types, CA has numerous co-benefits including reduced fuel consumption and increased soil C sequestration. Mechanical tillage is an energy-intensive process [41] and its reduction or elimination can decrease consumption of fossil fuels. For example, conversion from plow tillage (PT) to CA can reduce diesel consumption by as much as 41 L/ha [42].
In addition, an increase in SOC pool under CA can occur in soils not prone to accelerated erosion, and those which have optimal management strategies. A modeling study in Western Kenya showed

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that site-specific optimal management strategies can lead to SOC pool of 20 to 40 Mg/ha in 0.1 m depth and corn grain yield of 3.5 to 4.2 Mg/ha [43]. The most desirable tillage systems are those which restore soil quality, minimize risks of soil erosion, improve use efficiency of rain water and fertilizers [44] and minimize risks of SOC and nutrient depletion. Impacts of CA on soil quality restoration, an example of an upward spiral, is outlined in Figure 4.

Figure 4. Increase in soil resilience and mitigation of soil degradation by conservation agriculture (CA). Meta-analyses and any other comparisons among unrelated soil management practices can lead to misinterpretation of SOC sink capacity by CA [45] and erroneous inferences on agronomic productivity [46]. The mission is to identify site-specific packages of CA practices to make it functional (INM = integrated nutrient management).
Indiscriminate use of plowing, coupled with excessive removal of crop residues and unbalanced use of chemical fertilizers, can degrade soil quality, deplete SOC pool, and aggravate risks of soil erosion (Figure 2). In contrast, conversion of plow/traditional tillage to CA, especially on sloping lands and those vulnerable to accelerated erosion by water and wind under conventional management, can be

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conservation-effective, reverse degradation trends, and set-in-motion soil restoration processes with an upward spiral (Figure 4). Retention of crop residue mulch, and incorporation of a cover crop (forages) in the rotation cycle while eliminating bare fallows, can conserve soil and water and improve SOC pool in the surface layer (Figure 4). Increases in soil biodiversity, MBC and activity of earthworms and termites can all improve aggregation and encapsulate C within stable micro-aggregates as outlined in the hierarchy concept [47]. Strengthening elemental cycling, in conjunction with coupled cycling of C and H2O, can increase the solum’s C sink capacity and soil profile depth through increased bioturbation by earthworms or termites, and use of deep-rooted plants such as pigeon pea (Cajanus cajan), townsville stylo (Stylosanthes humilis (Kunth) Hester), or alfalfa (Medicago sativa). Long-term (>10 years) soil quality improvement will increase net biome productivity, improve water and nutrient use efficiencies, and increase above and below-ground biomass-C within the ecosystem. Progressive improvements in rhizospheric processes, driven by biotic mechanisms, would restore soil quality and mitigate degradation (Figure 4). It is important to note, however, that CA is a holistic and system-based approach. Mere elimination of plowing, while removing an excessive amount of crop residues and biomass for other uses (e.g., biofuels, industrial purposes) is not CA, and is rather an extractive farming system with negative impacts on soil and the environment. Thus, comparative analyses of un-related datasets can lead to erroneous assessments of SOC sink capacity associated with a properly implemented CA system [45] and misinterpretation of agronomic yields [46]. Furthermore, improvements in soil quality require more than the input of new varieties and chemical fertilizers [48]. The real issue is improving physical, biological and ecological components of soil quality, and set-in-motion an upward spiral eventually leading to social and political stability and international security (Figure 4).
6. Soil Fertility Management to Restore Soil Quality
Sustainable intensification (SI), producing more from less by reducing losses and increasing the use efficiency, is attainable only through improvement of soil quality including chemical quality or soil fertility. Although not the only way to increase soil fertility, the use of INM is a very effective approach for achieving SI. Nutrient depletion and loss of soil fertility are major causes of low productivity [49] in many developing countries. Use of organic amendments, by recycling organic by-products including urban waste, is a useful strategy to enhance soil fertility [50], and improve structural stability or aggregates [51]. While, nitrogen (N) input is important to improving soil fertility, its improper and/or excessive use can also lead to environmental pollution. China consumes about 30% of the world’s N fertilizer [52], and is able to feed ~22% of the world population on just 6.8% of the global cropland area. However, the country has severe environmental problems because of low N use efficiency, leaching of reactive N into surface and groundwater resources, and emission of N (as N2O) into the atmosphere.
7. Soil Quality and Water Resources
High soil quality or a healthy soil provides the foundation for a healthy economy, environment, and terrestrial biosphere. Thus, there exists a close link between soil quality and water resources in close proximity, such as the health of coastal ecosystems [53]. Changes in land use often affect water quality

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and pollutant loading [54,55]. Off-site movement of agricultural chemicals is often a significant source of non-point pollution. Many of the major rivers in countries with emerging economies have severe water pollution, contamination and eutrophication problems [56]. Downstream areas are often adversely affected because of adhoc agricultural development activities upstream. Among the most important adverse impacts are river desiccation, ground water depletion, surface and ground water pollution, accelerated erosion, sedimentation, salinization, and nutrient depletion [57]. These problems are especially severe in densely populated regions (e.g., East Asia, South Asia). Rapid urbanization, industrialization and increases in water demand have created severe water quality problems and degradation of the Ganges [58]. Land use changes induced by urbanization have had strong impacts both on soil and water quality in northern Iran [54]. Release of P from agricultural sources to streams and rivers has become a major factor affecting surface water quality not only in China [59], but also in the Great Lakes of North America (e.g., algal bloom of 2014). In Thailand, agriculture [especially rice (Oryza sativa) farming] is the key nutrient source within the Thachin River Basin [56]. Recent industrialization and community development have exacerbated water pollution and habitat degradation in the Gulf of Thailand [60]. The problem has been exacerbated by a rapid decrease in mangrove forest, coral reefs, and fishery resources due to misuse and mismanagement.
Irrigated agriculture, an important management strategy for high agronomic productivity in arid and semi-arid regions, is a mixed blessing. Mismanagement of irrigation waters has exacerbated problems with saline-sodic soils which now occupy more than 20% of the irrigated lands [61]. Furthermore, arid wetlands are also prone to contamination by sub-surface agriculture irrigation and drainage as in the Western USA [62]. These areas often experience toxicity problems in fish and wildlife due to drainage of water contaminants. In response, provisions must be made to reduce the amount of contaminants entering wetlands, and to provide for better allocation of freshwater between agriculture and wildlife [62]. Salinity problems are also often confounded by the reuse of untreated waste water (gray/black water) in agriculture [63], especially in urban areas prone to water shortages or those having water resources of marginal quality.
Restoring soil quality within managed ecosystems is critical to improving and sustaining water quality. To accomplish this goal, it is essential to develop strategies for integrated management of soil and water resources because of their strong inter-connectivity or the soil-water-waste nexus. While integrated water management alone is useful [64], the importance of the soil-water nexus cannot be over-emphasized [24]. Management of sediments, especially contaminated ones [65], is another important component of the soil-water nexus that must be critically examined.
8. Strategies for Soil Quality Restoration
Restoring the quality of degraded soils is a challenging task, especially in regions dominated by small, resource-poor landholders. Re-carbonization of the depleted SOC pool, which is essential to numerous functions, requires regular input of biomass-C and essential elements (i.e., N, P, and S) [66]. Thus, restoration of soil quality is a societal, national and international task that necessitates a coordinated approach.
There are three basic strategies of restoring soil quality (Figure 5): (i) minimizing losses from the pedosphere or soil solum; (ii) creating a positive soil C budget, while enhancing biodiversity; and (iii)

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strengthening water and elemental cycling. There is no silver bullet or panacea to accomplish these basic tasks, and site-specific factors (biophysical, social, economic, cultural) play a significant role. Some examples of site-specific, RMPs are outlined in Table 1. However, each of these technologies has their own tradeoffs, which must be duly considered and minimized.

Figure 5. Three strategies of restoring and managing soil quality for mitigating risks of soil degradation.

Strategy
Litter turnover
Forestry Plantations Woodlot Islets
Soil Carbon Sequestration Integrated Nutrient Management
Nutrient Management for SOC Sequestration Manuring
Residue Retention as Mulch
Regular Organic Inputs
Urban Waste
Soil Biological Management
Environmental Awareness

Table 1. Strategies to improve soil quality.

Region
Tropics
Tropics Degraded drylands Agroecosystems

Process The rate of organic matter and C supply
and nutrient cycling reactivation Silvo-pastoral system for nutrient cycling
Silvo-pastoral systems in drylands Optimal management strategies

Sub-Saharan Africa

Soil quality management

Sub-Tropical Red Soils (China)
Indus Plains Mexican Highlands
Western Kenya
Mediterranean Europe
Global soils
U.S.

Soil carbon buildup
Application of farm manure Improvement of soil structure
Nutrient retention and soil structure improvement Enhancing soil fertility
Enhance ecosystem services provisioned by SOC pool
Promoting technology adoption

Reference [3] [67] [68] [69] [17]
[70] [71] [72] [43,73] [16,74] [15] [75]
Soil QualitySoc PoolSoilSoil DegradationDegradation