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Manual timekeeping can be a daunting task, especially if you have many employees to monitor because you are part of a big organization or company. However, the task of keeping track of your employees attendance need not be difficult for you. Fortunately, there are different timekeeping software available in the web today which you could use for this job. Below is a list of our top ten timekeeping software choices based on features and usability: 1. It does its job well and has no project limits, which means that you can use it for as long as you like. It has also a simple interface and all its recorded data can be exported to Excel. Invoicera. Image courtesy of designwebkit. Invoicera is a premium Web- based timekeeping application that features a stopwatch- style timekeeping. It can monitor the time spent by employees on certain projects. Apart from its timekeeping capabilities, this program also has a built- in invoicing, expense logging and task list tools. It can seamlessly integrate with Base. Camp, as well as, with payment gateways such as Pay. Pal. This software is considered one of the best. Toggl. Image courtesy of asianefficiency. Toggl has many similar functions with Invoicera, such as its stopwatch timekeeping feature and invoicing tools. One of its advantages is its capability of integrating not only with Basecamp, but also with Quick. Books. Its data can also be exported to Excel. Although it is Web- based, it has desktop widgets for mobile devices such as the i. Phone. Toggl is a time keeping software ideal for employees who are timed on a per- task or per- project basis. It is a very easy to use program. Once a task is started, you can simply click on it and then click again once the task is complete. Harvest. Image courtesy of getharvest. Harvest is a feature- rich application that does stopwatch or timesheet time keeping. The data recorded can be exported to Quick. Books, Excel or Google Docs. It can also integrate with popular business applications such as Basecamp, High- rise and Quick. Books. Harvest is accessible through the Web and has widgets for desktop computers and the i. Phone. One of its prominent features is enabling you to log time by sending SMS or a direct message from Twitter to your phone. Many people consider this time keeping software powerful and efficient. Time. Card Manager. Image courtesy of brothersoft. Time. Card Manager is an application that is suitable for small businesses with up to 2. It replaces mechanical time clocks and automatically provides reports on employee hours worked and calculated earnings. This application can be installed in a single computer or in a network. Using this application, you can easily manage timekeeping and the payroll of your employees. Fresh. Books. Image courtesy of jurispage. Fresh. Books is a popular accounting program with timekeeping features. It can record time through stopwatch or a timesheet. It also comes with comprehensive features for invoicing and expense tracking. It has an API that allows the software to integrate with other programs like Salesforce, Basecamp and Mail. Chimp. This application is highly customizable. You ill certainly find this program of great value. Time. Click. Image courtesy of timeclick. With 1. 8 reporting options, Time. Click is one of the timekeeping applications that allow you to generate different kinds of reports. With this application, employees can simply clock in or out using any computer in the network. It also lets you set up an admin area where you can remotely manage the time logged by each employee. Time Clock MTSImage courtesy of downloadastro. With Time Clock MTS, you can turn an employees. It eliminates buddy punching, allowing a more accurate timekeeping for payroll. Using this application, your payroll staff will not have to manually tally time cards because it will automatically generate reports on the number of hours and minutes each employee has worked for a certain day. Shop. Clock. Image courtesy of shopclock. HourGuard Timesheet Software Time tracking software to log time on customer projects HourGuard makes it easy to track work hours with its simple-to-use interface. Click Start when you begin work, and Stop when you finish—the time tracking software does. DCAA Compliant Timekeeping Software. Simple QuickBooks Sync and QuickBooks Inegration. If you’re looking for reliable and simple to use timekeeping software, you've come to the right place. Popular downloads for timekeeping productivity software. This category includes reminders, desktop clocks, alarm clocks, etc. This is a program that enables the PC to connect to the outside world, by using the printer and parallel port LPT1. Shop. Clock is another feature- rich timekeeping program ideal for businesses that maintain up to three time shifts with different account titles for each shift in the general ledger. You could preset the time when each shift begins for proper payroll accounting. This application has a number of special features that make time keeping easier, such as, per day or per week subtotal on the time card grid of each employee, call lights for alerting administrators for any problem in logging, and a calendar report showing the scheduled time offs of employees. Realtime Advanced with PC Time Clock Lite. Image courtesy of sundialtime. Realtime Advanced is an application that works with PC Time Clock Lite. The PC Time Clock Lite is another program that allows employees to use their computers to monitor their number of hours worked per day. It is not a standalone application because it works with Realtime Advanced to gather its data and process them for payroll. Realtime Advanced has a powerful API which allows it to integrate with a wide spectrum of programs. The 1. 0 timekeeping software applications mentioned above are among the commonly used programs by many businesses for tracking their employees. Some of them are ideal for small businesses, while others can be used for medium- size or large businesses. If you have experience using any of the software applications listed above, please let us know in your comment. Or, if we missed out on your favorite time keeping software, we would certainly want to hear from you.? This interesting blog post is from Vagueware. ClockingIT – Free Timekeeping Software 0 By Garima on July 22, 2010 Business Software Productivity Software Editor Ratings: User Ratings: Our team has compared the best time card software of 2016. See up-to-date comparisons, reviews & costs for the top rated programs. 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The elements surrounding oxygen in the periodic table, nitrogen, fluorine, phosphorus, sulfur and chlorine, all combine with hydrogen to produce gases under standard conditions. The reason that water forms a liquid is that oxygen is more electronegative than all of these elements with the exception of fluorine. Oxygen attracts electrons much more strongly than hydrogen, resulting in a net positive charge on the hydrogen atoms, and a net negative charge on the oxygen atom. These atomic charges give each water molecule a net dipole moment. Electrical attraction between water molecules due to this dipole pulls individual molecules closer together, making it more difficult to separate the molecules and therefore raising the boiling point. This attraction is known as hydrogen bonding. The molecules of water are constantly moving in relation to each other, and the hydrogen bonds are continually breaking and reforming at timescales faster than 2. The liquid phase is the most common among water's phases (within the Earth's atmosphere and surface) and is the form that is generally denoted by the word . The solid phase of water is known as ice and commonly takes the structure of hard, amalgamated crystals, such as ice cubes, or loosely accumulated granular crystals, like snow. For a list of the many different crystalline and amorphous forms of solid H2. O, see the article ice. The gaseous phase of water is known as water vapor (or steam), in which water takes the form of a transparent cloud. When water achieves a specific critical temperature and a specific critical pressure (6. K and 2. 2. 0. 64 MPa), the liquid and gas phases merge to one homogeneous fluid phase, with properties of both gas and liquid. A likely example of naturally occurring supercritical water is in the hottest parts of deep water hydrothermal vents, in which water is heated to the critical temperature by volcanicplumes and the critical pressure is caused by the weight of the ocean at the extreme depths where the vents are located. This pressure is reached at a depth of about 2. These two unusual properties allow water to moderate Earth's climate by buffering large fluctuations in temperature. According to Josh Willis, of NASA's Jet Propulsion Laboratory, the oceans can absorb one thousand times more heat than the atmosphere without changing their temperature much and are absorbing 8. Of common substances, only that of ammonia is higher. This property confers resistance to melting on the ice of glaciers and drift ice. Before and since the advent of mechanical refrigeration, ice was and still is in common use for retarding food spoilage. Al in all of the forms studied, as Table 1 shows, produces harmful effects in living organisms: it especially harms the CNS. In studies involving in vitro cultures of. This table is provided as an information service by Diversified Enterprises. This table highlights the viscosity and surface tension of a variety of. Physics 9826b February 11, 13, 2013 1 1 Lecture 7 X-ray Photoelectron Spectroscopy (XPS) 7. Photoemission Spectroscopy (XPS) 7.1 Principles. Water is the chemical substance with chemical formula H 2 O; one molecule of water has two hydrogen atoms covalently bonded to a single oxygen atom. The specific heat capacity of ice at . Ice still floats in the oceans, otherwise they would freeze from the bottom up. However, the salt content of oceans lowers the freezing point by about 1. This is why, in ocean water, the downward convection of colder water is not blocked by an expansion of water as it becomes colder near the freezing point. The oceans' cold water near the freezing point continues to sink. So creatures that live at the bottom of cold oceans like the Arctic Ocean generally live in water 4 . This ice floats on the surface, and the salt that is . This denser salt water sinks by convection and the replacing seawater is subject to the same process. This produces essentially freshwater ice at . The increased density of the sea water beneath the forming ice causes it to sink towards the bottom. On a large scale, the process of brine rejection and sinking cold salty water results in ocean currents forming to transport such water away from the Poles, leading to a global system of currents called the thermohaline circulation. Miscibility and condensation. On the other hand, water and most oils are immiscible usually forming layers according to increasing density from the top. This can be predicted by comparing the polarity. Water being a relatively polar compound will tend to be miscible with liquids of high polarity such as ethanol and acetone, whereas compounds with low polarity will tend to be immiscible and poorly soluble such as with hydrocarbons. As a gas, water vapor is completely miscible with air. On the other hand, the maximum water vapor pressure that is thermodynamically stable with the liquid (or solid) at a given temperature is relatively low compared with total atmospheric pressure. For example, if the vapor's partial pressure is 2% of atmospheric pressure and the air is cooled from 2. The reverse process accounts for the fog burning off in the morning. If the humidity is increased at room temperature, for example, by running a hot shower or a bath, and the temperature stays about the same, the vapor soon reaches the pressure for phase change, and then condenses out as minute water droplets, commonly referred to as steam. A gas in this context is referred to as saturated or 1. Because the amount of water vapor in air is small, relative humidity, the ratio of the partial pressure due to the water vapor to the saturated partial vapor pressure, is much more useful. Water vapor pressure above 1. At the zero- pressure limit, the compressibility reaches a minimum of 6. As the pressure is increased, the compressibility decreases, being 6. The low compressibility of water means that even in the deep oceans at 4 km depth, where pressures are 4. MPa, there is only a 1. This point is used to define the units of temperature (the kelvin, the SI unit of thermodynamic temperature and, indirectly, the degree Celsius and even the degree Fahrenheit). As a consequence, water's triple point temperature, as measured in these units, is a prescribed value rather than a measured quantity. This pressure is quite low, about . The atmospheric surface pressure on planet Mars is 6. Pa, which is remarkably close to the triple point pressure. The altitude of this surface pressure was used to define zero- elevation or . Gustav Heinrich Johann Apollon Tammann in G. Kamb and others documented further triple points in the 1. It can remain in a fluid state down to its homogeneous nucleation point of about 2. K (. Water undergoes auto- ionization in the liquid state, when two water molecules form one hydroxide anion (OH. If water has even a tiny amount of such an impurity, then it can conduct electricity far more readily. It is known that the theoretical maximum electrical resistivity for water is approximately 1. M. A salt or acid contaminant level exceeding even 1. In ice, the primary charge carriers are protons (see proton conductor). The structure has a bent molecular geometry for the two hydrogens from the oxygen vertex. The oxygen atom also has two lone pairs of electrons. One effect usually ascribed to the lone pairs is that the H. The lone pairs are closer to the oxygen atom than the electrons sigma bonded to the hydrogens, so they require more space. The increased repulsion of the lone pairs forces the O. Due to the difference in electronegativity, there is a bond dipole moment pointing from each H to the O, making the oxygen partially negative and each hydrogen partially positive. In addition, the lone pairs of electrons on the O are in the direction opposite to the hydrogen atoms. This results in a large molecular dipole, pointing from a positive region between the two hydrogen atoms to the negative region of the oxygen atom. The charge differences cause water molecules to be attracted to each other (the relatively positive areas being attracted to the relatively negative areas) and to other polar molecules. This attraction contributes to hydrogen bonding, and explains many of the properties of water, such as solvent action. These properties include its relatively high melting and boiling point temperatures: more energy is required to break the hydrogen bonds between water molecules. In contrast, hydrogen sulfide (H2. S), has much weaker hydrogen bonding due to sulfur's lower electronegativity. H2. S is a gas at room temperature, in spite of hydrogen sulfide having nearly twice the molar mass of water. The extra bonding between water molecules also gives liquid water a large specific heat capacity. This high heat capacity makes water a good heat storage medium (coolant) and heat shield. Proposed structures. Other molecules like hydrogen fluoride, ammonia and methanol can also form hydrogen bonds. Download FREE Windows 7 themes, Wallpapers and Gadgets! We have the best custom Aero and Mac Windows 7 desktop themes, lots of nice tutorials and daily news. How to Uninstall / Remove Custom 3rd Party Themes in Windows? Windows 1. 0 Transformation Pack 6. Free Download - Freeware. Files. com. 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The problem is that it is such a guessing game of just how long we need to wait after one particular body part in order for the next time we hit that area for it to be effective. The larger body parts (legs, chest, back) are usually done over two days. Whereas arms, for example, are done over several days so they can be killed but not OVER KILLED for max gains. I am also a football coach and our strength training program is using this workout right now. Try this workout for at least 4 months and then take a short break (a few weeks) from the high intensity training before continuing. The Gym Workout. Terms You'll Need To Know: Failure - That point in an exercise at which you have so fully fatigued your working muscles that they can no longer complete an additional repetition of a movement with strict biomechanics. You should always take your post- warm- up sets at least to the point of momentary muscular failure, and frequently past that point. Learn More About Reading Workout Logs*3. Sets (4. 7 min)1. 10 Minute Workout: Short, Intense Workout To. Intense Workout provides FREE weightlifting workout routines. Best Muscle Building Workout, Diet & Exercises; The 5 Best Supplements For Muscle Gain. Conclusion . Good luck and may the Lord bless all your efforts! Day Workout Plan. DESCRIPTION The following 5 day workout routine is based on a 5 day split. Using this routine, you will train one bodypart per day for a duration of 5 days. There are two main advantages to using this type of routine. Firstly, you can train the body part with all out effort and intensity. You don't have to worry about training two or more body parts per session. Also, this type of program will allow for additional training volume (more sets and exercises). Secondly, it will allow for a longer period of rest. Training one body part per week will allow maximum rest and recuperation periods. By increasing the overall intensity of the program it will be necessary to increase the rest and recuperation periods (which this program does). Based on the volume of this type of routine, it is recommended that only advanced trainers use this type of program. If you are a beginner or intermediate, please see our 5 day beginner program here. Here is the training sequence: Day 1: Legs Day 2: Chest / Abs Day 3: Back Day 4: Shoulders / Abs Day 5: Biceps / Triceps Day 6: Rest (Cardio Optional) Day 7: Rest. Let's take a look at the workout. Workout Points. Duration: 5 to 6 weeks Goal: Increase muscle mass by allowing maximum recuperation for each body part. Method: - 5 workouts weekly. Several exercises per body part- Holistic repetition ranges - low, medium and high repetition range- Spill over routine set up. Each body part is worked once directly, once indirectly- Variable rest periods - matching repetition scheme- Cardio work at the end of each workout - 2. Notes. You can either use two or one days rest at the end of the training sequence. I recommend two at first and as you progress, try using one day. However, you will have to . Weight Increments: Try and add heavier weight to each progressive set (pyramid style). Once you are able to complete all repetitions on your last set (unassisted), increase the weight by 1. Rest: As indicated below, rest the recommended time in between sets. Once an exercise is complete, immediately set up and perform the next exercise. The Workout. Try and give this routine at least 5 weeks. If you find its working, stay with the program until it stops working. Click here for a printable version of this workout. Includes a workout log. For general workout logs, please see this page here. To find the amount of weight you need to be using, please use the one repetition maximum tool here. If you have any questions about this program, please email me at: buildingmuscle. Ask The Expert! 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