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To verify soil profile and N-SPT valuesoiloil exploration was done on 4 four) selected locations in Bantul regency.
Reduction of root diameter in response to low P availability, a process termed "root etiolation", has been suggested to reduce the metabolic cost of soil exploration (Lynch 2011).
As a part of geotechnical investigations one of the most common field tests, the standard penetration tests (SPT), was conducted for soil exploration.
While large lateral roots could be useful to increase the range of soil exploration for patches of greater phosphorus availability, they would also be more costly to construct, since they have larger diameter and length.
Increased specific root length, a phenomenon often observed under low nutrient treatments (Hill et al. 2006; Fernandez and Rubio 2015), is also predicted to reduce the cost of soil exploration (Chimungu and Lynch 2015).
We review our understanding of the molecular mechanisms that control this process in primary roots, and discuss recent insights into the regulation of oblique growth in lateral roots and its impact on root-system architecture and soil exploration.
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Successful use of soil in exploration for Cu oxide deposits in Mount Isa requires a genetic discrimination between residual and transported origin.
Concerning the latter, the BS001 genome also contained genes that potentially encode secondary metabolite biosynthesis, which is useful for highly competitive situations that may occur in the soil upon exploration for colonization space.
Furthermore, waterlogging significantly reduces root penetration, and thereby resumption of deep root growth may be of great importance for exploration of soil nutrients and water after the waterlogged soil has been drained (Thomson et al. 1992).
Research related to exploration of soil bacteria which can utilize the chemical surfactant in agriculture soil as carbon source can be another alternative to this environmental problem.
Since P is diffusion-limited and depletion zones develop around existing roots, continuous exploration of soil is important for P acquisition.
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