在火星号着陆地点发现碳酸的证据
W V Boynton1, D W Ming, S P Kounaves
1Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA. wboynton@LPL.Arizona.edu
概括
碳酸在火星土壤中被发现,表明过去的液态水活动. 这一发现提供了火星上古代水存在的证据,对于了解火星地质历史至关重要.
科学领域:
- 行星科学 行星科学
- 天体生物学 天体生物学
- 地质化学 地质化学
背景情况:
- 碳酸盐是行星表面过去水性过程的关键指标.
- 了解火星的地质历史依赖于确定过去水的证据.
- 之前的任务已经寻找了火星上水和可居住性的证据.
研究的目的:
- 为了识别和量化火星土壤中的碳酸在星着陆地点附近.
- 为了确定形成条件和检测到的碳酸对过去火星水的历史的影响.
主要方法:
- 扫描热量计被用来检测矿物学过渡.
- 在大约725°C时对内热过渡和二氧化碳演变的分析.
- 评估土壤pH缓冲能力,防止添加酸.
主要成果:
- 碳酸在火星土壤中被确定为3-5重量百分比的碳酸.
- 这种矿物质在725°C左右呈现出内热过渡,并释放出二氧化碳.
- 土壤表现出显著的pH缓冲能力.
结论:
- 碳酸的存在和数量与大气二氧化碳与表面液态水膜的相互作用形成一致.
- 这一发现强烈支持了火星表面过去液态水活动的假设.
- 结果为火星的古代气候和潜在可居住性提供了宝贵的见解.
更多相关视频
08:09Measuring and Mapping Patterns of Soil Erosion and Deposition Related to Soil Carbonate Concentrations Under Agricultural Management
Published on: September 12, 2017
11:19Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
Published on: October 21, 2016
相关概念视频
Porosity in Cement Paste
The porosity of concrete is a measure of the void spaces within its structure. These spaces impact its strength and durability significantly. When water and cement interact, a chemical reaction called hydration creates a semi-solid paste. This paste includes combined water, making up approximately 23% of the cement's dry mass, and gel water, which fills minuscule voids known as gel pores, accounting for about 28% of the cement gel volume.
The balance of water to cement in the mix is critical—it...
The balance of water to cement in the mix is critical—it...
Minerals
Minerals are essential nutrients that the human body needs in small amounts to work properly. They play a vital role in many bodily functions, such as building strong bones and transmitting nerve impulses. Some minerals are needed for hormone production or to maintain a normal heartbeat. Major minerals include calcium, phosphorus, potassium, sulfur, sodium, chlorine, and magnesium, while trace minerals include iron, manganese, copper, iodine, zinc, cobalt, fluoride, and selenium.
The Fossil Record
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
The Evidence for Evolution
Genetic variations accumulating within populations over generations give rise to biological evolution. Evolutionary changes can result in the formation of novel varieties and entire new species. These changes are responsible for the diverse forms of life inhabiting the planet. The evidence for evolution suggests that all living organisms descended from common ancestors.The collection of fossils within sedimentary rocks give a record of common ancestry and often depicts the history of evolution.
Skeleton and Calcium Homeostasis
Calcium is not only the most abundant mineral in bone but also the most abundant mineral in the human body. Calcium ions are needed for bone mineralization, tooth health, heart rate regulation and strength of contraction, blood coagulation, the contraction of smooth and skeletal muscle cells, and the regulation of nerve impulse conduction. The average calcium level in the blood is about 10 mg/dL. When the body cannot maintain this level, a person will experience hypo or hypercalcemia.
Carbon Skeletons
Life on Earth is carbon-based, as all macromolecules that make up living organisms contain carbon atoms. All organic compounds have a carbon backbone. Each carbon atom is tetravalent and can bond with four other atoms, making it an extraordinarily flexible component of biological molecules. Because carbon’s valence electrons are stable, it rarely becomes an ion. As the carbon chain increases in length, structural modifications such as ring structures, double bonds, and branching side chains...
