The Kafue Flats Experience

By Dave Lowry, Tim and Trish Broderick, Musa Lambakasa, James France, Stéphane Baugitte
Photos by Tim and Trish Broderick and Dave Lowry

The first ZWAMPS campaign consisted of both aircraft and ground surveys, these being linked most closely in the Kafue Flats region over the period Feb 2 to 5. The Kafue Flats are a floodplain wetland, extending from Itezhi-Tezhi Dam in the west, some 240 km east to Kafue town and never more than 50 km wide (https://en.wikipedia.org/wiki/Kafue_Flats). The river has changed course many times across its plain leaving scattered oxbow lakes and isolated snake-like sections of meanders to stagnate outside of flood season (Fig. 1).

Fig. 1 River Kafue lakes and meanders.

Fig. 1 River Kafue lakes and meanders.

The surveys and sampling commenced on Saturday with an intensive 4-hour zigzag flight over the region, designed by Keith Bower (Fig. 2), with elevated methane noted toward the eastern end near the start of the flight, before vertical mixing reduced these signals. The flight was very much enjoyed by Tim and our Zambian Ministry of Mines group, including Musa. Separating out the wetland source from the flight measurements and isotope data will be quite difficult because there were also numerous rural cattle herds and very extensive burning plumes producing methane (Fig. 3).

Fig. 2 End of the zig-zag flight

Fig. 2 End of the zig-zag flight

Fig. 3 Biomass burning plumes close to river

Fig. 3 Biomass burning plumes close to river

On Sunday we attempted to find our way by road to the northern margin of the Kafue Flats through the Blue Lagoon national park. After a 3-hour drive from Lusaka we reached a faded sign saying Nakeenda Lodge 9 km.  The national park sign was even more rusted. Soon we realised that this part of the park had not been visited for a long time as the track became more an overgrown and very muddy path, so we decided to sample air from a dambo in the pristine savanna (Fig. 4). The site was full of butterflies of numerous species, and even a praying mantis was catapulted into the car as we brushed past the luxuriant vegetation (Fig. 5).

Fig. 4 Stéphane directing air sampling

Fig. 4 Stéphane directing air sampling

Fig. 5 Mantis on water bottle

Fig. 5 Mantis on water bottle

Undeterred we decided to approach the park from the NW corner and reached a barrier. Here the head park ranger directed us to the managed game area and wetland.  After a few kilometres we turned off along a narrow track not on maps or GPS. Then followed 20 km over 90 minutes down a narrow and churned up track. As we passed across the invisible park boundary we came to a fishing camp on a rise above the floodplain and its associated biting insects. We were greeted by excited children and an ox cart (Fig. 6). Turns out that we were still some kilometres from the river, the resident lechwe antelope or the Game Ranger patrol camp. At this point we realised we had to get back to Lusaka before dark.

The return was no quicker, especially being interspersed with air sample collection in the pristine national park grassland (Fig. 7), as we carefully traced our way back along interweaving tracks using the GPS. We approached the outskirts of Lusaka as night fell, and on a road without lighting, carefully negotiated many minibuses without lighting and pedestrians bustling across the road to lively markets. Alarm bells had been ringing back at base when we failed to arrive back for the evening briefing and our Blue Lagoon destination was all that was known. As the city approached and phone reception returned we were able to let all know we had not broken down in the bush.

Fig. 6 Ox cart and children in the camp

Fig. 6 Ox cart and children in the camp

Fig. 7 Musa and Dave fishing for air

Fig. 7 Musa and Dave fishing for air

On Monday we had planned to sample on the south side of the floodplain, overnight in the Relax Hotel in Monze and then meet up with Mike Daly at the Lochinvar hot springs on Tuesday, but after breakfast Tim noticed that the Ford had a rear puncture from our toils the previous day, which fortunately hadn’t materialised on the evening drive back. Tim headed off hoping for a quick fix, but a brake fluid leak was also discovered from a distorted and corroded seal. Many discussions and calls later a replacement vehicle was delivered at 6 in the evening.

Plans quickly changed and the proposed rendezvous with Mike was scrapped due to the long distance, and the focus for Tuesday was to get into the sugar cane plantations and wetlands near Mazabuka. All was fine until about 2 hours into the drive when, on probably the steepest hill climb on the Kafue-Livingstone main road, there was a load bang from the rear of the vehicle. This time a major blow out and a 3 cm long rip in the tyre. Tim and Musa got to work on the jack while we jammed the other wheels with some lovely roadside calc-silicate boulders. Convoys of lorries heading for Botswana and South Africa laden with copper and other goods struggled past us. It soon became apparent that the supplied jack was not high enough for our Landcruiser, but we managed to flag down a local farmer and get the change done.

That’s when we noticed a 1cm diameter, perfectly round hole through the alloy wheel below the rip in the tyre, with a very clear entry and exit direction from a high velocity impact (Figs. 8 and 9). None of us had seen anything like that before and we still don’t know the cause, so we will leave this to your imagination.

Fig. 8 Hole in the alloy wheel – inside view

Fig. 8 Hole in the alloy wheel – inside view

Fig. 9 Hole in the alloy wheel – outside view

Fig. 9 Hole in the alloy wheel – outside view

At Mazabuka we found a tyre repairperson and then followed a wild goose chase to find a welder, then through sugar cane plantations to a market for electrodes, which then didn’t work because the alloy was wrong and required a DC current. After 2 more lost hours, we had a reality check, dumped the wheel and tyre into the back and decided to risk it on the spare and take the 30 km of dirt tracks NE toward the wetlands and river. With co-ordination of aerial images and GPS we headed down a narrow track and finally came to lush vegetation, reed beds (bulrushes) and clusters of water lilies, before the track stopped abruptly in a small clearing populated by a group of fisher folk. We proceeded to collect air samples from different heights in the reed beds. In the midst of this the reeds seemed to part and a small canoe cruised into the bank laden with good-sized Kafue bream (Figs. 10 and 11).

Fig. 10 Boatmen in the reed beds

Fig. 10 Boatmen in the reed beds

Fig. 11 Cargo of Kafue bream

Fig. 11 Cargo of Kafue bream

The drive back was far less eventful. The next morning the car hire people inspected the wheel and seemed overly keen to give us our deposit back and get us on our way. We can certainly look back on a couple of eventful and somewhat surreal days that we won’t forget in a hurry and hope that the few highly prized air samples were well worth our efforts to collect them.

Bagsy the Air Samples: Life on the aircraft for the isotope bag sampling

James France and his sack of bags

James France and his sack of bags

Unlike quite a lot of the science on board the FAAM aircraft, the high precision carbon isotopes in methane have to be done back at the lab at Royal Holloway. To make this happen, we have to collect bags of air mid-flight as we pass over areas of interest, trying to capture the range of sources in the flight plan. However, it does mean that our role can look at little bit budget compared to the needs of a complex and expensive instrument rack measuring species in real-time during the flights.

The life of the isotope sampling team depends on your point of view… The instrument scientist who has to turn up 4 hours before take-off sees the isotope sampler swanning onto the aircraft at the last minute, switching on a pump and a laptop and writing some sticky labels. The logistics team who despair after each flight as we hand over a massive sack containing around 20 bags of air and ask them to find somewhere to store them and then ship them back home. The crew who just hear calls on the radio from the less technically named “bags”. Suggested nicknames which have fortunately not gained traction include “Team Bags”, “Dr Bag” and “Bag Man”…

I prefer to think us more of an Ngolo Kante or Anders Herrera (Ed – can we have a football reference in a science blog?). It’s not altogether obvious what we contribute until all the data is looked at, well after the campaign is done.

Collecting the air

It really is a simple as it sounds. The FAAM aircraft is fitted a large air inlet line which directs air from outside the aircraft to the various instruments, and the bag sampler has a pump which allows air from the outside to be directed in to the bags. The bags are made by SKC, and have been demonstrated in the laboratory to hold the methane without any leaks for months at a time, which gives us plenty of time to do the analysis. To show the full complexity of it, I agreed to do a special with plenty of detail for an upcoming edition of the Barometer podcast run by the University of Manchester.

In order for us to get useful data to identify the source we need to collect a suite of samples at as large a range of concentrations of methane as possible, fortunately the aircraft is well equipped and can measure atmospheric methane concentration in real-time. We use this information to try to sample the air into the bags at the most scientifically useful points.

Why are we interested?

As I’m sure you’ve read on many other posts on this blog and others, methane is rising globally and we’re not entirely sure why… One of the possible reasons is an increase in emissions from tropical wetlands, so we’re on this campaign to try and gather information needed such as the isotopic source signature and the flux of methane being emitted from tropical methane sources. There’s a lovely new paper (shameless plug) which has just been accepted which looks at the impact of methane globally “Very strong atmospheric methane growth in the four years 2014 – 2017: Implications for the Paris Agreement” which will be available in the journal Global Biogeochemical Cycles soon…

We’ll keep the blog updated with something later in the year, once the laboratory analysis has started to take shape.

by James France

On the aircraft, “Team Bags” is James France, Rebecca Fisher and Dave Lowry of Royal Holloway University Earth Science Department.

On the ground, a separate but co-ordinated with the aircraft, sampling campaign is ongoing with Tim Broderick, Trish Broderick and Dave Lowry.

Papyrus: a methane emitter and natural wind vane

The papyrus swamp measurements team
Tue 22 January 2019
Part 1

Having planned out the next few days flights – to lakes/wetlands as well as fires – and with no point refining the plans based on the weather forecast because we don’t know exactly when we will be able to start flying, I’ve joined Rebecca again to do some air sampling. This time with intent, and with a full rucksack containing anything I might need (unlike yesterday).

We are currently in a taxi out to see a contact, Steve Forsyth, who works at Mission Aviation Fellowship – Uganda, and is based at an airfield by a papyrus swamp. MAF is an organisation that operates small aircraft to transport refugees from nearby countries like the Democratic Republic of Congo or Sudan. The swamp will be a source of methane and so will be a good opportunity to work out the carbon-13 fingerprint of such an ecosystem. The principal investigator of this project, Euan Nisbet, has sampled here before, so it will be good to find out whether the fraction of carbon-13 varies over time or is very consistent.

Getting out of the conference room is a good chance to stop obsessing over ever evolving weather forecasts and see some of Uganda. And I can make myself useful by taking photos of the sampling location at very least.

Part 2

We are on the way back from the airfield now. It was completely surrounded by papyrus swamp, which meant we could access it quite easily. We were escorted around the airfield by Ivan, who was essential in helping us not get our feet wet (we were not keen to lose a trainer in the swamp!) while getting as close to the swamp as possible.

The papyrus plants were extremely tall in places – close to 4m probably. Some areas were cut down to the stem, and they grow back in about a month according to Ivan. The stems themselves are very strong, and are excellent wind vanes of you ever are in need of one. Which I did, as I was taking wind measurements to accompany the air samples.

In all, we took 13 samples from locations close to the surface of the water up to about 2m high, all around the edge of the swamp, plus one background sample further away from it. This will allow us to find out the carbon-13 fingerprint of this papyrus swamp, where there were the highest methane concentrations. For example, the papyrus that was cut down to ground level may emit more or less methane than the fully grown area and maybe the measurements will give us an indication of that.