Spains Hall Estate (SHE), a farm in south-east England, have established a completely new model of farming including forest restoration, agroforestry, biodiversity-friendly farming methods and farming for ecosystem services, including natural flood management. It is a superb example of how land can provide both high value crops for the market and a range of ecosystem services as public goods . Policysupport.org (King's College London and AmbioTEK) have worked with Spains Hall Estate since 2019, monitoring and modelling the meteorological, hydrological and biodiversity baseline and helping understand landscape processes and the environmental benefits of the farming interventions made.
Spains Hall Estate, riparian grassland
During the 20th Century at SHE, in common with most UK agricultural land, ditches were cleared, field drains installed, fields ploughed, ponds filled and hedgerows removed, in response to market forces and the subsidy regime in place. This led to reduced natural flood storage and increased flashiness of streamflow as well as impacts on biodiversity and other ecosystem services. Since 2016, farm subsidies in England have been increasingly targeted towards the delivery of public goods (ecosystem services including natural flood management), thereby reducing incentives for such intensification of production.
Finchingfield village
The village of Finchingfield, just downstream of SHE is a picturesque settlement at a crossroads of some regionally important rural roads. The Finchingfield Brook, that drains SHE, has flooded this crossroads during extreme events, for example in 2014. Natural Flood Management interventions at SHE since 2019 have targeted the elimination of these floods.
Spains Hall Estate, beaver-felled tree
Beavers were reintroduced in an enclosure in March 2019 to help in natural flood management and to create wet woodland, a rare habitat in the UK. A larger enclosure was completed in 2023 to allow beavers to take over the maintenance of a series of eight leaky debris dams also installed in 2019. Beavers build and maintain networks of dams and wetlands that slow-the-flow which can reduce flood peaks downstream. We have monitored the hydrological impact of these interventions throughout.
Spain's Hall Estate is actively engaged in several environmental initiatives:
Natural Flood Management: The estate employs natural flood management techniques, such as use of leaky debris dams, beaver re-introduction and reforestation, to reduce flood risks. These methods enhance water retention and slow runoff, protecting downstream communities.
Biodiversity Net Gain: By restoring habitats (e.g. woodland and wet woodland) and incorporating nature into farming systems (e.g. herbal leys), Spain's Hall Estate contributes to biodiversity net gain, including the generation of some 500 BNG credits.
Countryside Stewardship: Participating in Countryside Stewardship schemes, the estate adopts sustainable farming practices, hedgerow planting, and field margin management to enhance wildlife habitats.
Agroforestry: The estate is developing the largest agroforestry project in Europe. This farming system is more resilient than arable to climate drying, provides high value nut crops, improves soil health, increases carbon sequestration, provides shade for other crops and enhances overall farm resilience.
Agriculture: The estate employs nature-friendly agricultural techniques for more sustainable food production, environmental conservation and nature recovery.
Our research at Spains Hall Estate has been ongoing since 2019, funded by H2020 NAIAD and H2020 ReSET and involves the development of environmental intelligence for understanding strategy and effectiveness assessment for nature-based solutions. This involves intensive digital monitoring using www.FreeStation.org open source monitoring systems and detailed spatial modelling using WaterWorld and Co$tingNature. The current network of monitoring stations is shown in the map below. Activities include:
Monitoring streams and ditches to better understand the source areas for water and the dynamics of streamflow in relation to rainfall, land cover and soil properties;
Monitoring the impact of natural flood management interventions — including leaky debris dams and beaver re-introduction — on flood peaks, dry season flows and water quality;
Monitoring of weather and its variability in time and space across the estate, including measurement of novel metrics such as instantaneous rainfall rates;
Monitoring of soil moisture dynamics across the estate and the impact of different farming practices on soil moisture. Monitoring of moisture dynamics in agroforestry systems and the potential for drought impacts of tree growth;
Monitoring of biophony using acoustic monitoring methods, for better understanding spatio-temporal variation of audio-ecological surrogates for biodiversity.
Modelling the effectiveness of natural flood management (NFM) interventions in reducing flood peaks, with WaterWorld/local
Mapping the ecosystem services provided by SHE using Co$tingNature/local
Left: Summary of monitoring activities, video produced by Sheetal Martine Joseph. Above: Spains Hall Estate FreeStation monitoring network. S = soil moisture; l = stream level, flow, W = weather station
Long term temperature trend
These data from nearby Rothamsted (57km away) show recent temperature trends (1920-2024) as anomalies from the mean over the period, highlighting a mean temperature increase of ~1 deg. C over the period. This will have a direct impact on crop growth but also increase evapotranspiration by about 2–5%, depending on factors like humidity, vegetation, and soil moisture. Data: Met Office via recent/climate.
Long term trend of days with rainfall
The long term trend of number of rainfall days from the same nearby station shows a reduction of around 5 rainfall days per year over the period. Combined with increases in evapotranspiration this may lead to greater dry season soil moisture deficits and production challenges for rainfed, shallow-rooting annual crops such as cereals. Data: Met Office via recent/climate.
Long term trend of rainfall per rainday
Rainfall per rain-day is a measure of rainfall intensity. The data show a clear trend of increasing rainfall intensity over time since the 1980s. This concentration of rainfall in fewer raindays increases the risk of flooding as catchment stores of water saturate and rainfall rates overwhelm rates of infiltration of water into soil. Data: Met Office via recent/climate.
We have >26 long-term data loggers in place, making SHE one of the most intensively monitored farms in the world. These dataloggers are our own www.freestation.org designs and record data every 10 mins to characterise meteorology, hydrology and audio-ecology at SHE. As developers of the FreeStation technology, we have also tested and perfected a number of new FreeStation prototypes at SHE. We have also developed an instance of Co$tingNature/local and WaterWorld/local at 10m spatial resolution for SHE. Co$tingNature/local maps nine ecosystem services (wildlife services to cropland - pollination and pest control; grazing and fodder services; carbon storage and sequestration, fuelwood, water pollution dilution; natural flood storage; water resource provision; urban cooling and soil erosion mitigation) and helps to understand nature's benefits to people. Example data are shown below.
Monitored tributaries of SHE
This map from Co$tingNature/local shows the monitored sub-catchments of the Finchingfield Brook. The beaver projects cover the small catchments to the south-west and, more recently, the mainstem catchment.
Live weather station data, with forecast
Our www.freestation.org live weather stations measure rainfall, temperature, humidity, air pressure, solar radiation , wind speed and wind direction. They also connect with a global forecast model (GFS) to deliver 5 day forecasts for some of these variables. Here we see measured and forecast temperature and rainfall.
Greatest per-pixel ecosystem service provision across SHE
The map from Co$tingNature/local shows the most significant ecosystem services (benefits of nature) at SHE are pollution dilution (blue); grazing and fodder (yellow); natural flood storage (brown) and carbon storage and sequestration (grey).
To date, our research as part of the H2020 NAIAD and H2020 ReSET projects has focused on the development of low-cost, open source environmental sensors, dataloggers and networks of sensors and their application to environmental intelligence. Having developed a reliable, accurate, maintainable and integrated network of sensors our current work is focused on using data from the network to better understand the impacts of interventions at SHE on biodiversity and ecosystem services. With the data collected so far, we have shown that:
Most (~75%) of the flow to Finchingfield originates in the main Finchingfield Brook with ~11% from the beaver stream and some ~14% from the East Stream (outside of SHE). Some 22% of flow originates in the upper sub-catchment of the Finchingfield Brook (also outside of SHE).
The leaky debris dams installed in 2019 have been effective in reducing flood risk to Finchingfield since they have restored the floodplain function of the brook, causing it to overflow during extreme events, flooding the surrounding riparian grassland, instead of the village just downstream.
The 2019 Beaver reintroduction has created a new wet woodland with at least 1.66 ha of wetland storing 1.66 m3 of water for each 1cm of water depth. During an extreme event in the winter such as Storm Henk (2024) this wetland is capable of storing 7.5% of the water generated by the area upstream. The much larger beaver enclosure on the Finchingfield Brook has, within two years, created significant areas of wetland on this much more significant stream. Though beaver dams do breach, as a result of water overflow or treefall, they are rapidly repaired ensuring their role in natural flood management is maintained long-term.
Soil moisture dynamics in the agroforestry plots show very high spatial variability within and between fields. They dry out significantly in the summer, particularly near the surface and from July to September.
Beaver dam breach and re-build in 2019 beaver enclosure pounds
These water level data from the 2019 beaver enclosure ponds show a dam breach resulting from treefall onto the dam. Water level in the pound falls by 13cm over 60 minutes. The beavers repair the dam over 130 minutes and the pound takes a further 250 minutes to fill.
Water storage in beaver wetland during storm Henk (2024)
Storm Henk at SHE rained for 16 hours with a storm rainfall total of 4.88mm, producing 187,930 m3 of water over the catchment. Of this, as shown by the line on the figure, some 846 m3 of storm water was temporarily held back by the 2019 beaver wetlands, representing 7.5% of storm water produced over the beaver enclosure catchment.
Soil moisture dynamics in agroforestry plantations (20cm depth)
These data show the challenges of growing shallow-rooting, rainfed annuals, such as cereals, in south-east England. Soil moisture near the surface dries quickly during periods without rainfall, reaching lows of 20-30% by volume in places for 2-3 weeks. The deeper-rooting perennial tree crops that make up an agroforestry system are exposed to much more stable soil moisture regimes at depth.