Recently I’ve been mentoring a PhD candidate through their first ever manuscript to be submitted to a journal which involves determining porosity of a material with a heterogeneous pore structure. The technique we were using relied on adsorption of nitrogen at 77 K on to the surface of pores within the material. As we went on this journey, I got the impression that we had very different approaches to our work and this made me question what it takes to be a scientist: the attitudes and behaviors that come so easily to some do not seem to manifest in others. What does it mean to be a scientist and how has this influenced materials science?
We are curious
Science is about following the evidence, asking why, and finding information on the things you don’t understand. We design experiments to investigate these things and improve our understanding. We base that investigation on a question. When we design an experiment, we think about all of the factors that could affect the outcome and we decide how we can control them. We carefully consider all of the details while drawing on our experience and scientific instinct. We are careful and thoughtful.
Dewar and Ramsay appear to be the first to report on the sorption of nitrogen and other gases at low temperature. Their separate studies, reported in 1905 and 1906, focused on the composition of the atmosphere and the separation of noble gases. Their simple curiosity about the air around them kicked off a whole series of experiments that ended up being very useful for analyzing porous materials.
We strive for understanding
Science is personal. It’s about developing your own understanding and passing it on to others. Rather than glossing over the details, pretending that they’re not important to us and that someone else will take care of them, we leap on the details and turn them over in our minds; we examine them from all angles to decide their importance in our experiments. We push them together with other details and look at how they fit together. We search books and journals to help us with the details and then list everything that we still do not know.
After the first reported gas sorption studies in the 1900’s, Langmuir went on to develop a model for ideal localized monolayer adsorption (1916) that later allowed Brunauer, Emmet and Teller to publish a theory which supported the calculation of surface area (1938). Later, the Kelvin equation was used by Barrett, Joyner and Halenda to arrive at a very popular method for finding the pore size distribution (1951). The work of one scientist or group built on the work of another, each body of work inspiring someone to ask a new question.
The International Union of Pure and Applied Chemistry initially categorized adsorption isotherms into 6 different types (King et al, 1985), which was recently refined to closely relate them to pore structures (Thommes et al, 2015).
We are transparent and honest
We make assumptions. Once we’ve pulled together this vast body of knowledge, collected by hundreds of scientists over many decades, we look at what is still unknown and as ourselves what is logical: following all of the evidence, what could be a sensible possibility? We state these assumptions clearly and loudly so that others can understand our reasoning. We invite others to test our assumptions. We communicate our logical argument with straightforward prose, carefully defining our assumptions.
Langmuir very clearly pointed out that his model relates to a flat plane where all adsorption sites are uniform. Similarly, Brunauer, Emmet and Teller specified that their theory assumes that the completed monolayer is made of close-packed spheres. For nitrogen, each sphere is usually said to cover an average area of 0.162 nm2. To calculate the Brunauer-Emmet-Teller (BET) surface area, the theory should only be applied to a part of the adsorption isotherm that matches some consistency criteria, and these criteria depend on both the adsorbent and adsorptive as well as temperature. To determine pore size, we assume that the pores are rigid and all of the same simple shape with the curvature of the meniscus dependent only on the dimensions of the pores. It is generally agreed that this method is not applicable to micropores (<2 nm in width) and only applicable to macropores (>50 nm) if the conditions can be extremely well controlled.
Rearranging the BET equation allows a straight line to be plotted so that the BET parameters can be found. The section of the isotherm to which the BET fit is applied must meet the consistency criteria, indicated on the graph by the red data points.
We use high-tech equipment and know how it works
Much of this understanding, scientific evidence, theory and basic physics, and even some assumptions are packaged into high precision instruments – tools that we can use to delve even deeper into science and answer yet more challenging questions.
There is a plethora of equipment out there that will automatically program nitrogen sorption at different relative pressures, and will even calculate the BET surface area and pore size distribution. These results should be carefully scrutinized. Many will default to applying the BET theory to relative pressures of 0.05 – 0.35, but of course, you should check the applicability to your material before relying on the default calculation.
To sum up: We are curious; we are inspired. We are scientists.
This article draws on a review paper by Kenneth Sing “The use of nitrogen adsorption for the characterization of porous materials”, Colloids and Surfaces A: Physicochemical and Engineering Aspects 187–188 (2001) 3–9 as well as various forum discussion on ResearchGate.