Biochar: A Synthesis of Its Agronomic Impact beyond Carbon SequestrationKurt A. Spokas, Keri B. Cantrell, Jeffrey M. Novak et al.|Journal of Environmental Quality|2012 Biochar has been heralded as an amendment to revitalize degraded soils, improve soil carbon sequestration, increase agronomic productivity, and enter into future carbon trading markets. However, scientific and economic technicalties may limit the ability of biochar to consistently deliver on these expectations. Past research has demonstrated that biochar is part of the black carbon continuum with variable properties due to the net result of production (e.g., feedstock and pyrolysis conditions) and postproduction factors (storage or activation). Therefore, biochar is not a single entity but rather spans a wide range of black carbon forms. Biochar is black carbon, but not all black carbon is biochar. Agronomic benefits arising from biochar additions to degraded soils have been emphasized, but negligible and negative agronomic effects have also been reported. Fifty percent of the reviewed studies reported yield increases after black carbon or biochar additions, with the remainder of the studies reporting alarming decreases to no significant differences. Hardwood biochar (black carbon) produced by traditional methods (kilns or soil pits) possessed the most consistent yield increases when added to soils. The universality of this conclusion requires further evaluation due to the highly skewed feedstock preferences within existing studies. With global population expanding while the amount of arable land remains limited, restoring soil quality to nonproductive soils could be key to meeting future global food production, food security, and energy supplies; biochar may play a role in this endeavor. Biochar economics are often marginally viable and are tightly tied to the assumed duration of agronomic benefits. Further research is needed to determine the conditions under which biochar can provide economic and agronomic benefits and to elucidate the fundamental mechanisms responsible for these benefits.
Management Controls on Soil CarbonFarmers have long recognized the organic matter content of a soil as a key attribute of soil fertility. The development of agriculture in temperate regions has exhibited patterns of exploitative soil use followed by the introduction of regenerative practices as soil resources fell to unacceptable levels. In the simplest terms, the level of soil organic carbon (C) in a soil will be governed by the difference between inputs of organic matter and outputs through mineralization, erosion, and leaching. The controls on decomposition processes are, in most respects, more complex and less easily manipulated by management than are inputs of organic matter. Climate and soil differences constrain management options and thereby determine which practices are most important in affecting soil C. Plant residues are the major source of C inputs in all terrestrial ecosystems. The history of agriculture is replete with examples of the depletion of organic matter and the subsequent loss of soil fertility through poor management.
The effect of young biochar on soil respirationUnderstanding and Enhancing Soil Biological Health: The Solution for Reversing Soil DegradationOur objective is to provide an optimistic strategy for reversing soil degradation by increasing public and private research efforts to understand the role of soil biology, particularly microbiology, on the health of our world’s soils. We begin by defining soil quality/soil health (which we consider to be interchangeable terms), characterizing healthy soil resources, and relating the significance of soil health to agroecosystems and their functions. We examine how soil biology influences soil health and how biological properties and processes contribute to sustainability of agriculture and ecosystem services. We continue by examining what can be done to manipulate soil biology to: (i) increase nutrient availability for production of high yielding, high quality crops; (ii) protect crops from pests, pathogens, weeds; and (iii) manage other factors limiting production, provision of ecosystem services, and resilience to stresses like droughts. Next we look to the future by asking what needs to be known about soil biology that is not currently recognized or fully understood and how these needs could be addressed using emerging research tools. We conclude, based on our perceptions of how new knowledge regarding soil biology will help make agriculture more sustainable and productive, by recommending research emphases that should receive first priority through enhanced public and private research in order to reverse the trajectory toward global soil degradation.
Long-Term Impacts Of Tillage, Fertilizer, And Crop Residue On Soil Organic Matter In Temperate Semiarid Regions