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Within the current research context, this setup has been uniquely designed to optimize inorganic carbon sequestration by enhancing mineral weathering through the activity of soil biota, while concurrently manipulating abiotic factors known for stimulating weathering. The possibility in this setup of collecting both the solid processed material and the leachate enables a full characterization of both fractions. Despite the enormous amount of columns, the collection of the samples and the analyses carried out ensure a high-quality data collection. Besides, having a large number of combinations in a single experimental run is very important for analyzing the collected data with modern and advanced statistical methods, such as machine learning. These methods can be used to determine the main variables leading to high weathering rates and further carbon sequestration. Consequently, this setup provides the opportunity to improve the understanding of the effects that soil organisms can have on EW and IC sequestration. This is fundamental to establishing more realistic constraints on the boundaries of EW and its efficiency in reducing atmospheric CO2 concentrations. This setup presents several originalities compared to existing studies investigating EW and the effect of soil organisms.
Regarding the effects of abiotic factors on EW, these have already been investigated in previous studies4,29,30,31,32,33,34. Some of these studies compared different amounts, types, and grain sizes of rocks, but their setup either consisted of a pot experiment32,33 or included mixing rock powder with soil34. Other experiments focused on one rock type with different irrigation rates but did not have the possibility of irrigating frequently with an automated system or focused on multiple irrigation rates and frequencies35. Other studies presented a setup similar to the one presented in the current protocol, with the possibility of adjusting irrigation rates and maintaining temperature constant, besides varying rock grain sizes and types29,30. Furthermore, the design of these setups was comparable to the one proposed in the present manuscript and designed to collect the leachate for further analyses29,30. Additionally, CO2 concentrations were varied in these studies as another factor enhancing weathering29. However, none of these previous studies have focused on the effect of biotic factors on promoting EW. In this setup, the aim is to enhance the weathering process, and further IC sequestration, by inoculating specific bacteria, fungi and earthworms and determining to which extent they can accelerate EW.
In relation to the effect of biotic factors on EW, few studies have not specifically focused on EW but have investigated whether soil organisms can influence mineral weathering. These studies have mainly explored how weathering is affected by soil organisms using culture mediums19,21, Petri dishes36, nylon bags buried in the soil14, or small amounts of rock powder mixed with other substrates36,37. Using such small systems or setups makes it challenging to disentangle the effect of organisms from other variables. Some experiments used a similar setup to the one here proposed but at a smaller scale, with rock powder-filled columns inoculated with soil organisms38,39,40. However, these experiments either concurrently grew plants and did not focus on the exclusive effect of specific soil organisms13,35, or did not collect the leachate36. Besides, most of the studies that showed that bacteria, fungi, and earthworms increase mineral weathering have focused on the effect of these organisms on nutrient release as an indication of weathering rather than on IC sequestration11,13,14,19,36,37,38. Above all, none of these earlier studies aimed at promoting EW or presented the possibility of adjusting and maintaining abiotic factors throughout the experimental period. In this setup, instead of keeping all abiotic factors constant, a multitude of combinations are tested for four abiotic factors, such as water irrigation rates and frequencies, rock powder type, and grain size, with the aim of promoting EW through soil organisms' activity.
Besides, none of the previous studies that have focused on the effect of either abiotic or biotic factors on EW presented the possibility of having an extremely large number of columns and variables within one experimental run. In this setup, it is possible to test multiple different combinations of various variables during one run of experiments due to the impressive number of columns for which the setup has been designed, while still providing high-quality results. Given the novelty of the setup, below some possible improvements and remaining challenges that could be considered while designing future similar setups are presented.
Homogenous air conditions in the incubation chamber should be ensured. The placement of the setup in a climate chamber ensured constant temperature and relative humidity. Ventilation constraints (e.g., air flow) may have created spatial variability in atmospheric conditions and thus led to disproportional evaporation from the columns at certain locations, which is a common phenomenon in this kind of setup35. To handle this drawback, when replication and randomization are not possible, it is advised to calculate a water balance for columns placed at various locations throughout the chamber.
The columns should be carefully aligned with the funnels once inserted into the acrylic plate to avoid leachate loss. During the experimental period considered, leachate losses occurred from the bottom of the columns due to an incorrect positioning of the funnels or due to the clogging of the meshes. Together with evaporation, this can partly explain why the leachate collected was lower compared to expectations (Figure 13). To minimize these losses, it is important to make sure that the funnels are optimally positioned below the columns. Using wider funnels is also a viable option. In this case, attention should be paid to the diameter of the holes during the construction of the acrylic plates and the distance between acrylic plates.
Slower water flow in soil column experiments where water is applied frequently is a recurrent issue7,30,40. In the experiments carried out with the presented setup, in some cases rather high irrigation rates and very fine mineral grain sizes were used, which initially lack a structure as normally observed in soils. This might have caused the pores of the meshes at the bottom of the columns only containing fine minerals to clog during the run of the experiments. Therefore, water did not flow fast enough through the columns, which resulted both in flooding of the columns, reducing water infiltration and leachate collection, and in anoxic conditions within the columns, impacting biogeochemical processes. To mitigate this issue, it is important to always mix a certain percentage of coarse with finer mineral grain sizes and to avoid 100% very fine mineral grain size mixtures. Another option is to allow is allow the columns to experience a certain number of wetting/drying cycles to initiate soil structure formation, and thus improve water infiltration. Besides, before the start of the experiment, it would be useful to determine basic soil water dynamics, such as saturated and unsaturated flow and water retention curve, in a few mesocosms to better understand gas flow, mineral saturation state and drivers of organisms' activity.
The presented experimental setup is convenient to use, presents a straightforward installation and can be adjusted according to research needs. In the context of mineral weathering, with the necessary adjustments, it can be coupled with a gas chamber in order not only to characterize carbon in the solid and aqueous phase but to look at the dynamics of carbon in the gas phase as well. Besides, this setup can be used to study realistic water infiltration rates with dry-wet sequences, as these temporal dynamics could strongly influence weathering41. The use of this setup is not limited to experiments that focus solely on silicate minerals, but it can be implemented in column experiments that use different substrates. Besides, the length of the experiments can be shortened or extended according to experimental needs, and the number of columns can be changed. The possibility of collecting samples from both the solid processed materials and the leachate allows us to carry out different analyses to focus on one of the two components or both. To present knowledge, this is the only setup that has been built so far with an exceptional number of columns that aims at using soil organisms to enhance mineral weathering while concurrently controlling abiotic conditions in a system made of solely silicate minerals and organic materials.