Multiscale Impacts of Cyanobacterial Crusts on Landscape Stability

蓝藻结皮对景观稳定性的多尺度影响

• 批准号: NE/K011626/1
• 负责人: Kevin White
• 金额: $ 26万
• 依托单位: University of Reading
• 依托单位国家: 英国
• 项目类别: Research Grant
• 财政年份: 2014
• 资助国家: 英国
• 起止时间: 2014 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=NE%2FK011626%2F1
• 关键词: Multiscale; Impacts; Cyanobacterial; Crusts; Landscape

Most soils are a mixture of inorganic (mineral) and organic (e.g. plant) material. In deserts, often there is not enough rain for large plants to grow, but organisms such as algae and lichens can survive. Our research focuses on cyanobacteria which live on or near the soil surface and produce sugars as they grow, called polysaccharides, which can stick small particles (e.g. sand grains), together. This binds the soil forming a 'cyanobacterial soil crust' that is helpful in the landscape because it makes it harder for soil erosion to take place. Cyanobacterial soil crusts occur naturally, but can also be made artificially as part of a land management plan. In deserts often soil erosion is caused by wind, however sometimes it rains causing water erosion, and the amount and intensity of rainfall affects crusts. Light rain causes cyanobacterial growth and helps to thicken and strengthen the crusts, but heavy rain can break up crusts, making them less able to protect soil from erosion. We know little about the relationship between different rainfall intensities and the ability of crusts to protect soil from wind and water erosion but it would be useful to do so because we could better plan activities such as where cattle graze (hooves break up weak crusts) and when to leave fields bare.This project is exciting because it studies the impact of rainfall, runoff (surface flow) and wind erosion on cyanobacterial crusts at different scales. To begin, we control conditions by growing crusts on an artificial soil bed under a rainfall simulator that lets us choose how much rainfall occurs, and how long it lasts. We also choose whether the soil bed is flat or sloping, and can control runoff rate. After the simulated rainfall, we will use a wind tunnel on top of the soil bed to simulate wind erosion - again we choose the wind speed and can measure how much soil is blown away. By doing this, we can test the response of cyanobacterial soil crust to different rainfall events (does the crust get thicker? is it broken up and washed away?) and we can measure how good the crust is at preventing wind erosion. Our approach is unusual because it looks at how one set of processes (rainfall and runoff) affects a second process (wind erosion). From this we will develop a model to explain and predict the impact of rainfall/runoff on soil crust growth and susceptibility to wind erosion. The model will then be tested in the field using natural soils and cyanobacterial crusts. To guarantee a range of rainfall and wind events, the field tests will be partially controlled using a portable field rainfall simulator and wind tunnel.Finally, the controlled experiments are conducted at a small scale but we will broaden the spatial and temporal scope of the project to the regional scale which is more applicable to understanding landscape stability. We will do this using remote sensing because aspects of cyanobacterial crust growth and development can be detected using satellite data. We will use these data to examine cyanobacterial crust response to rainfall and runoff (both also detectable from space) at the regional scale and monitor the time-lag between these hydrological inputs and dust storms to further test the model at larger spatial and temporal scales.Cyanobacteria occur in many environments, e.g. the protective crusts they form are important in temperate climates where they protect soil between crops from water erosion, and they form on coastal dunes, where they reduce sand transport by wind. Having developed and calibrated a model for predicting the impact of water on the protective role of crusts in drylands, we can test the model on other soils and under alternative rainfall patterns (e.g. temperate or tropical). Scientists have predicted that the amount and intensity of rainfall in many areas will change in the future; it will also be possible to use our model to try and predict how this will affect cyanobacterial crusts.

大多数土壤是无机（矿物）和有机（如植物）物质的混合物。在沙漠中，通常没有足够的雨水供大型植物生长，但藻类和地衣等生物可以生存。我们的研究重点是蓝细菌，它们生活在土壤表面或附近，并在生长时产生糖，称为多糖，可以将小颗粒（例如沙粒）粘在一起。这使土壤结合形成一个“蓝藻土壤结皮”，这是有益的景观，因为它使土壤侵蚀更难发生。蓝藻土壤结皮是自然产生的，但也可以作为土地管理计划的一部分人工制造。在沙漠中，土壤侵蚀通常是由风引起的，但有时也会下雨造成水侵蚀，降雨量和强度会影响结壳。小雨会导致蓝细菌生长，并有助于增厚和强化地壳，但大雨会破坏地壳，使其无法保护土壤免受侵蚀。我们对不同降雨强度与地壳保护土壤免受风和水侵蚀的能力之间的关系知之甚少，但这样做会很有用，因为我们可以更好地规划活动，例如在哪里放牧（蹄子打碎脆弱的外壳）以及什么时候让田地裸露。这个项目令人兴奋，因为它研究降雨的影响，径流（地表径流）和风蚀对蓝藻结皮的影响。开始，我们通过在降雨模拟器下的人工土壤床上种植结壳来控制条件，让我们选择降雨量和持续时间。我们还可以选择是否土壤床是平的或倾斜的，并可以控制径流率。在模拟降雨之后，我们将在土床顶部使用风洞来模拟风蚀-同样，我们选择风速，可以测量有多少土壤被吹走。通过这样做，我们可以测试蓝藻土壤结皮对不同降雨事件的反应（结皮会变厚吗？是不是被冲散了？）我们可以测量地壳在防止风蚀方面有多好。我们的方法是不寻常的，因为它着眼于一组过程（降雨和径流）如何影响第二个过程（风蚀）。由此，我们将开发一个模型来解释和预测降雨/径流对土壤结皮生长和风蚀敏感性的影响。然后，该模型将在现场使用天然土壤和蓝藻结皮进行测试。为了保证一定范围的降雨和风事件，现场测试将使用便携式现场降雨模拟器和风洞进行部分控制。最后，控制实验在小尺度上进行，但我们将扩大项目的时空范围，以更适用于了解景观稳定性的区域尺度。我们将使用遥感技术进行这项工作，因为可以使用卫星数据检测蓝藻结皮生长和发展的各个方面。我们将利用这些数据来研究蓝藻结皮对降雨和径流的响应（两者也可从空间检测），并监测这些水文输入和沙尘暴之间的时滞，以进一步在更大的空间和时间尺度上测试模型。例如，它们形成的保护性结壳在温带气候中很重要，在那里它们保护作物之间的土壤免受水侵蚀，并且它们形成在沿海沙丘上，减少了风对沙子的输送。在开发和校准了一个预测水对旱地结壳保护作用的影响的模型之后，我们可以在其他土壤和其他降雨模式（例如温带或热带）下测试该模型。科学家们预测，未来许多地区的降雨量和强度将发生变化;也有可能使用我们的模型来尝试和预测这将如何影响蓝藻结皮。

项目成果

The effect of biological crusts on soil response to raindrop impact

生物结皮对土壤雨滴冲击响应的影响

• 作者: Bullard J.E.

Wind erodibility response of physical and biological crusts to flood and rain

物理和生物结皮对洪水和雨水的风蚀响应

• 作者: Aubault, H.

High resolution measurements of soil surface roughness response to wind erosion and rainfall.

土壤表面粗糙度对风蚀和降雨响应的高分辨率测量。

• 发表时间: 2016
• 作者: Bullard J.E.

Development and testing of a micro wind tunnel for on-site wind erosion simulations

用于现场风蚀模拟的微型风洞的开发和测试

• DOI: 10.1007/s10652-016-9478-8
• 发表时间: 2016
• 期刊: Environmental Fluid Mechanics
• 影响因子: 2.2
• 作者: Strong C

Microbial transport and soil integrity in drylands.

旱地微生物运输和土壤完整性。

• 发表时间: 2017
• 作者: Elliott D.