Keep It 2.2.2
Keep It is for writing notes, keeping web links and documents, and finding them again. Available on Mac, and as a separate app for iPhone and iPad, Keep It is the destination for all those things you want to put somewhere, confident you will find them again later.
Keep It 2.2.2
2.2.2 Restricted Assets. The following concerns only Restricted Assets: Restricted Assets have license terms different from other Assets. Those license terms are found in the materials accompanying Restricted Assets ("Restricted Asset Terms"). For clarity, to the extent Restricted Asset Terms are different from this EULA, the Restricted Asset Terms will control; otherwise, this EULA will continue to apply. No other use is licensed or permitted and END-USER may otherwise not use, reproduce, publicly display, publicly perform, transmit, distribute, sublicense, rent, lease or lend Restricted Assets. Without limitation of the foregoing it is emphasized that END-USER shall not be entitled to share the costs related to purchasing a Restricted Asset and then let any third party that has contributed to such purchase use such Restricted Asset (forum pooling).
Temporary views in Spark SQL are session-scoped and will disappear if the session that creates itterminates. If you want to have a temporary view that is shared among all sessions and keep aliveuntil the Spark application terminates, you can create a global temporary view. Global temporaryview is tied to a system preserved database global_temp, and we must use the qualified name torefer it, e.g. SELECT * FROM global_temp.view1.
Based on user feedback, we changed the default behavior of DataFrame.groupBy().agg() to retain thegrouping columns in the resulting DataFrame. To keep the behavior in 1.3, set spark.sql.retainGroupColumns to false.
Airflow installation might be sometimes tricky because Airflow is a bit of both a library and application.Libraries usually keep their dependencies open and applications usually pin them, but we should do neitherand both at the same time. We decided to keep our dependencies as open as possible(in setup.cfg and setup.py) so users can install differentversion of libraries if needed. This means that from time to time plain pip install apache-airflow willnot work or will produce unusable Airflow installation.
What's weird about all of this is that I have a directory named shared inside of app/views. Inside there I have a file named _header.html.erb.I'm using Ruby 1.8.7, Rails2.2.2, and following the documentation found here.
A firm will be able to comply with SYSC2.2.1 R by means of records which it keeps for its own purposes providedthese records satisfy the requirements of SYSC2.2.1 R and provided the firm takes reasonable care to keep them upto date. Appropriate records might, for this purpose, include organisationalcharts and diagrams, project management documents,job descriptions, committee constitutions and terms of reference providedthey show a clear description of the firm's majorfunctions.
Sometimes when other quick attempts at debugging fail, you need a way to take a deeper look into your script. Most integrated development environments (IDEs) like Spyder include some debugging tools that allow you to step through your script line-by-line to attempt to find an error. These tools allow you to keep an eye on the value of all variables in your script to see how they react to each line of code. The Debug toolbar can be a good way to catch logical errors where an offending line of code is preventing your script from returning the correct outcome. The Debug toolbar can also help you find which line of code is causing a crash.
Can you spot the error now? The fact that the loop has failed to exit should draw your attention to the loop condition. The loop will only exit when "multiplier" is greater than or equal to "number." That is obviously never going to happen as "number" keeps getting bigger and bigger as it is multiplied each time through the loop.
Click the Stop button the Debug toolbar to end the debugging session. We're now going to step through a corrected version of the factorial script, but you may notice that the Variable Explorer still displays a list of the variables and their values from the point at which you stopped executing. That's not necessarily a problem, but it is good to keep in mind. In fact, you could go to the Console and type print(number) to see that those variables are still held in Spyder's memory.
We can represent the stoichiometrically equivalent phthalic anhydride plus water by keeping the same atom block and changing a couple of entries in the bonds block. Now, we have one connection table (MOL III) representing two molecules. (Connection tables can also be used in representing reactions. For more on this, see online documentation on MOL and related file formats.)
This sentence has several interesting aspects that we need to decide whether to keep or to ignore when tokenizing. The first issue is the contraction in "Don't", which presents us with several possible options. The fastest option is to keep this as one word, but it could also be split up into "do" and "n't".
The next issue at hand is how to deal with "$1"; the dollar sign is an important part of this sentence as it denotes a kind of currency. We could either remove or keep this punctuation symbol, and if we keep the dollar sign, we can choose between keeping one or two tokens, "$1" or "$" and "1". If we look at the default for tokenize_words(), we notice that it defaults to removing most punctuation including $.
Information lost to tokenization (especially default tokenization) occurs more frequently in online and more casual text. Multiple spaces, extreme use of exclamation characters, and deliberate use of capitalization can be completely lost depending on our choice of tokenizer and tokenization parameters. At the same time, it is not always worth keeping that kind of information about how text is being used. If we are studying trends in disease epidemics using Twitter data, the style the tweets are written in is likely not nearly as important as what words are used. However, if we are trying to model social groupings, language style and how individuals use language toward each other becomes much more important.
WorkFirst staff combine the participant's resources with what the program can provide. For example, if a participant has a car repair need that costs $700 so they can keep their job, the participant and the worker may find out from the vendor how much of the cost could be paid in installments if the program paid for a large portion of the repair up front.
The following topic describes the steps to migrate your existing Apache Airflow workload to a new Amazon MWAA environment. You can use the following steps to migrate from an older version of Amazon MWAA to a new version release, or migrate your self-managed Apache Airflow deployment to Amazon MWAA. This tutorial assumes you are migrating from an existing Apache Airflow v1.10.12 to a new Amazon MWAA running Apache Airflow v2.2.2, but you can use the same procedures to migrate from, or to different Apache Airflow versions.
After you have made the required changes to your workflow resources, checkout the v2.2.2 branch of the aws-mwaa-local-runner repository, and test your updated workflow DAGs, requirements, and custom plugins locally. If you're migrating to a different Apache Airflow version, you can use the appropriate local runner branch for your version, instead.
HTTP/1.1 states that HTTP connections can be re-used for multiple requests per default. HTTP/1.0 compliant endpoints can also use a mechanism to explicitly communicate their preference to keep connection alive and use it for multiple requests. HTTP agents can also keep idle connections alive for a certain period time in case a connection to the same target host is needed for subsequent requests. The ability to keep connections alive is usually refered to as connection persistence. HttpClient fully supports connection persistence.
The HTTP specification does not specify how long a persistent connection may be and should be kept alive. Some HTTP servers use a non-standard Keep-Alive header to communicate to the client the period of time in seconds they intend to keep the connection alive on the server side. HttpClient makes use of this information if available. If the Keep-Alive header is not present in the response, HttpClient assumes the connection can be kept alive indefinitely. However, many HTTP servers in general use are configured to drop persistent connections after a certain period of inactivity in order to conserve system resources, quite often without informing the client. In case the default strategy turns out to be too optimistic, one may want to provide a custom keep-alive strategy.
This software package should install on any reasonable machine running a 32 or 64bit version of Windows 2000, XP, Vista or Windows 7/8. Testing has only been performedon machines running with the latest service packs installed. For this reason, you areencouraged to keep your operating system up to date when using this software. An accountwith administrative privileges will be required to run the install application but notfor normal operation.
2.1.1 Soil compositionWhen dry soil is crushed in the hand, it can be seen that it is composed of all kinds of particles of different sizes.Most of these particles originate from the degradation of rocks; they are called mineral particles. Some originate from residues of plants or animals (rotting leaves, pieces of bone, etc.), these are called organic particles (or organic matter). The soil particles seem to touch each other, but in reality have spaces in between. These spaces are called pores. When the soil is "dry", the pores are mainly filled with air. After irrigation or rainfall, the pores are mainly filled with water. Living material is found in the soil. It can be live roots as well as beetles, worms, larvae etc. They help to aerate the soil and thus create favourable growing conditions for the plant roots (Fig. 26).Fig. 26. The composition of the soil2.1.2 Soil profileIf a pit is dug in the soil, at least 1 m deep, various layers, different in colour and composition can be seen. These layers are called horizons. This succession of horizons is called the profile of the soil (Fig. 27).Fig. 27. The soil profileA very general and simplified soil profile can be described as follows:a. The plough layer (20 to 30 cm thick): is rich in organic matter and contains many live roots. This layer is subject to land preparation (e.g. ploughing, harrowing etc.) and often has a dark colour (brown to black).b. The deep plough layer: contains much less organic matter and live roots. This layer is hardly affected by normal land preparation activities. The colour is lighter, often grey, and sometimes mottled with yellowish or reddish spots.c. The subsoil layer: hardly any organic matter or live roots are to be found. This layer is not very important for plant growth as only a few roots will reach it.d. The parent rock layer: consists of rock, from the degradation of which the soil was formed. This rock is sometimes called parent material.The depth of the different layers varies widely: some layers may be missing altogether.2.1.3 Soil textureThe mineral particles of the soil differ widely in size and can be classified as follows:Name of the particlesSize limits in mmDistinguisable with naked eyegravellarger than 1obviouslysand1 to 0.5easilysilt0.5 to 0.002barelyclayless than 0.002impossibleThe amount of sand, silt and clay present in the soil determines the soil texture.In coarse textured soils: sand is predominant (sandy soils).In medium textured soils: silt is predominant (loamy soils).In fine textured soils: clay is predominant (clayey soils).In the field, soil texture can be determined by rubbing the soil between the fingers (see Fig. 28).Farmers often talk of light soil and heavy soil. A coarse-textured soil is light because it is easy to work, while a fine-textured soil is heavy because it is hard to work.Expression used by the farmerExpression used in literaturelightsandycoarsemediumloamymediumheavyclayeyfineThe texture of a soil is permanent, the farmer is unable to modify or change it.Fig. 28a. Coarse textured soil is gritty. Individual particules are loose and fall apart in the hand, even when moist.Fig. 28b. Medium textured soil feels very soft (like flour) when dry. It can be easily be pressed when wet and then feels silky.Fig. 28c. Fine textured soil sticks to the fingers when wet and can form a ball when pressed.2.1.4 Soil structureSoil structure refers to the grouping of soil particles (sand, silt, clay, organic matter and fertilizers) into porous compounds. These are called aggregates. Soil structure also refers to the arrangement of these aggregates separated by pores and cracks (Fig. 29).The basic types of aggregate arrangements are shown in Fig. 30, granular, blocky, prismatic, and massive structure.Fig. 29. The soil structureWhen present in the topsoil, a massive structure blocks the entrance of water; seed germination is difficult due to poor aeration. On the other hand, if the topsoil is granular, the water enters easily and the seed germination is better.In a prismatic structure, movement of the water in the soil is predominantly vertical and therefore the supply of water to the plant roots is usually poor.Unlike texture, soil structure is not permanent. By means of cultivation practices (ploughing, ridging, etc.), the farmer tries to obtain a granular topsoil structure for his fields.Fig. 30. Some examples of soil structures GRANULAR BLOCKY PRISMATIC MASSIVE 2.2 Entry of water into the soil 2.2.1 The infiltration process 2.2.2 Infiltration rate 2.2.3 Factors influencing the infiltration rate 041b061a72