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Vaniria Setser
This calculator converts cholesterol units from the popularly used mg/dL to the SI units mmol/L. It works for total serum cholesterol, high-density lipoproteins (HDL), low-density lipoproteins (LDL), and triglycerides.
It looks like you just had your cholesterol levels checked. If you're interested in using them to assess your heart disease risks and general health condition, check out our cholesterol ratio calculator.
The American Heart Association (AHA) recommends that all adults age 20 or older have their cholesterol checked every four to six years and work with their healthcare providers to determine their risk for cardiovascular disease and stroke.
Input the value in either the first or second field based on your preference, whether you want to convert from mg/dL to mmol/L or vice versa. Alternatively, you can seamlessly switch between units of measurement.
For instance, consider a scenario in which you have a total serum cholesterol value of 200 mg/dL and wish to convert it to mmol/L using the cholesterol units converter. If you input the value 200 into the first field of the Total serum cholesterol, HDL, or LDL group, the calculator will provide an equivalent value of 5.172 mmol/L.
Motivated by my passion for providing precise and accessible tools for healthcare professionals and a broader audience, I designed the cholesterol units converter to aid individuals, including myself, in seamlessly converting cholesterol values. My dedication to facilitating understanding and informed decision-making in lipid profile interpretation is evident in the user-friendly design and functionality of the tool.
We prioritize the quality of our content, ensuring it is as accurate and reliable as possible. Each tool undergoes peer review by a trained expert and subsequent proofreading by a native speaker. If you would like to learn more about our standards, please refer to the the Editorial Policies page.
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1a. Photosynthesis is the process in which plants use solar energyto convert carbon dioxide and water into carbohydrates.Photosynthesis is important because it creates food and oxygen,necessary resources for the continuation of life on Earth. SeeSection 1.1.
2a. Respiration is the reverse of photosynthesis. Duringrespiration, stored energy is converted into available energynecessary for the maintenance and formation of cell material. This isnecessary for all metabolic processes. See Sections 1.1 and2.3.1.
2c. Food produced by photosynthesis forms the base of mostecosystem food chains. Herbivores eat plant material and carnivoreseat herbivores, gaining some energy from the foods they consume. Onlya fraction of the energy consumed at a lower level is carried to thenext level. See Section 2.1 and Figure 3.01.
3a. Plants are called primary producers because they produce thematerial and store the energy at the bottom of the food chain. Inother words, all animals are dependent, either directly or indirectlyon the food materials stored in plants. See Section 2.1 and Figure3.01.
3b. Gross primary production (GPP) is the total rate at whichmaterial is produced and net primary production (NPP) is the rate atwhich material is accumulated in excess of respiration. In otherwords, NPP is GPP minus respiration. See Section 1.2.
3c. No. Net primary production is directly related to ecosystemconditions. Ecosystems where the environment most favors plant growthand lower respiration rates will have the highest rates of NPP . SeeSection 1.2.
4a. Plants are important components of the hydrologic cycle. Theyact as physical buffers by slowing down the flow and impact of hardrain, while their roots help to bind soil. This helps the soil toabsorb more water and inhibits erosion. Vegetation uptakes, stores,and eventually releases water back into the atmosphere by the processof transpiration (also known as evapotranspiration). See Section 2.2and Figure 3.02.
5a. Carbon is the most abundant element in the nonwater portionsof plants (about 50%). As vegetation grows, carbon is taken from theatmosphere and stored in plants. When a plant decays or is burned,this carbon is released back to the atmosphere and the soil. SeeSection 2.3.1 and Figure 3.03.
6a. Yes. Human activities can significantly modify the naturalpathways of energy flow and biogeochemical cycles. This includeschanging amounts of elements stored and released to various Earthrealms, alteration of nutrient and energy flow pathways, depletionand removal of soils, disruption and destruction of habitats, anddecreased diversity in plant and animal communities. See Section3.1.
6b. Production is maximized in agricultural systems, but requiresmore energy and water input than natural ecosystems to sustainyields. Monocultural crops are generally more susceptible to diseaseand insect attack than natural ecosystems. See Section 3.2.
6c. Deforestation reduces biological diversity and increases waterrunoff and soil erosion. Deforestation also changes local andsometimes regional climate patterns by altering surface albedos, windspeeds, and latent heat cooling. Biomass burning releases carbondioxide, trace gases and particulates into the atmosphere. SeeSection 3.3
6d. Yes. When indirect usage of NPP is considered, the total ofglobal terrestrial NPP coopted by humans and domestic animals rangesfrom roughly 40-58%. This indirect appropriation of NPP by humans issubstantially disproportionate to direct use (3% of global NPP) byhumans. The more NPP humans coopt, the less available for naturalecosystems. See Section 3.1.
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