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Understanding soil health

Natural soil is an ecosystem consisting of minerals, organic matter (OM), living organisms, water, and air and maintaining an unceasing flow of matter and energy within and with the surrounding environment via various physical, chemical, and biological processes (Guo, 2021). It is also through these processes such as water retention, chemical oxidation, and microbial decomposition that natural soil functions to support plant growth, regulate water movement and purify water, decompose organic wastes and recycle nutrients, harbor organisms, and buffer environmental changes. The capability of a soil to perform these environmental functions and provide according ecosystem services, however, is determined by the efficiency of the soil to carry out the intrinsic physical, chemical, and biological processes under particular geographic and climate conditions and is indicated by “soil health” (Guo, 2021).

Soil health is defined as “the continued capacity of soil to function as a vital living ecosystem that sustains plants, animals, and humans.” A lengthier version of the definition is as “the capacity of soil to function as a vital living system, within ecosystem and land-use boundaries, to sustain plant and animal productivity, maintain or enhance water and air quality, and promote plant and animal health”. In brief, soil health indicates the capability of a soil to furnish ecosystem services. The health of a soil reflects how well the soil can carry out its environmental functions. A soil is evaluated “healthy” if it provides comparable or better ecosystem services relative to undisturbed reference soils of the similar type in the same region. Otherwise the soil is unhealthy, unable to perform the normal environmental functions of the like soils in the inherent ecosystem.

Soil health is a comprehensive expression of the relevant soil physical, chemical, and biological properties (Figure 1).
soil health expressing soil properties
Figure 1. Soil health as a comprehensive expression of various soil properties
The current concept of soil health was evolved in 1990s from “soil quality” referring to “the capacity of a soil to function within ecosystem and land-use boundaries to sustain biological productivity, maintain environmental quality, and promote plant and animal health.” The term was first mentioned by Mr. Henry A. Wallace in 1910 in an unpublished thesis to describe soil fertility (Guo, 2021). In 1936 USDA published a document entitled “Soil Health and National Wealth” to promote soil fertility and nutrient management. The U.S. farmers started to adopt the term in 1990s, motivating the scientific community to re-define soil health. The term became popular in the 2010s, presumably a result of the 2007–2008 global food crisis and the recognition of soil’s carbon (C) sequestration potential for mitigating climate change. The term declares that soil is a living entity in analogy with an organism or a community that can be evaluated by healthiness. As an ecosystem, soil can be healthy or unhealthy, depending on how well the ecosystem is maintained and its stability, resilience, and stresses are self-regulated.

The scientific system of soil health covers primarily three aspects: concept, assessment, and management (Figure 2).
scientific soil health system
Figure 2. Development of the science of soil health on concept, assessment, and management as the three focal areas. SMAF: Soil management assessment framework; CASH: Comprehensive assessment of soil health; SHAPE: Soil health assessment protocol and evaluation
The health status of an agricultural soils is illustrated by its actual capacity relative to that of a population of like soils in the same region for sustaining a satisfactory crop productivity through maintaining desirable nutrient cycles, soil structure, C transformation, and pest and disease regulations. Healthy agricultural soils are usually characterized by a higher-than-average crop productivity, sufficient supply of nutrients, appropriate OM contents, right tilth and drainage, dominating presence of beneficial organisms over pathogens, high resistance to erosion and degradation, and being contamination-free (Guo, 2021). Compared with less healthy ones, healthier soils generally demonstrate a wider working ranges and a higher input-to output conversion efficiency.

Soil (health) degradation is “the loss of the intrinsic physical, chemical, and/or biological qualities of soil either by natural or anthropic processes, which result in the diminution or annihilation of important ecosystem functions”. Land uses, disturbances, and management practices may alter soil properties and subsequently, impact soil health. Tillage, for example, deteriorates soil structure and promotes OM mineralization, leading to significant health degradation of cropland soil.

Healthy soil is the foundation of sustainable agriculture. To promote the vitality of soil and enhance the soil health of agricultural lands from the federal policy perspective, USDA-NRCS Soil Health Division was created in 2014. The Soil Health Institute was founded in 2016 as a U.S. non-profit organization to facilitate soil health research and scientific advancement. The European Commission formed the Mission Board for Soil Health and Food in 2019 to develop the interim targets and long-term goals on soil health and food as “ensure that 75% of soils are healthy by 2030 and are able to provide essential ecosystem services”. In Australia, the former Governor General has been appointed by the Minister for Agriculture and Water Resources since 2013 as the National Advocate for Soil Health to promote the science and practice of soil health in collaboration with the non-profit organization Healthy Soil Australia. Worldwide, an open, dynamic database (SoilHealthDB) has been initiated to collect and store global soil health data. The concept of soil health has been gradually embraced by farmers, soil conservationists, and policymakers around the world (Guo, 2021).

Guo, M. 2021. Soil health assessment and management: recent development in science and practices. Soil Syst. 5, 61. doi: 10.3390/soilsystems5040061

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Dr. Mingxin Guo
Department of Agriculture and Natural Resources
Delaware State University
1200 N. DuPont Highway
Dover, DE 19901
Email:mguo@desu.edu
Phone:+1 (302) 857 6479
Fax:+1 (302) 857 6405
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