alea-institute/kl3m-data-sample-004-shuffled huggingface dataset:
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#           Thermal infrared spectroscopy of experimentally shocked anorthosite and pyroxenite: Implications for remote sensing of Mars      

      January 1, 2002    

The feldspar and pyroxene mineralogies on Mars revealed by the Thermal Emission Spectrometer (TES) on Mars Global Surveyor likely record a variety of shock effects, as suggested by petrologic analyses of the Martian meteorites and the abundance of impact craters on the planet's surface. To study the effects of shock pressures on thermal infrared spectra of these minerals, we performed shock recovery experiments on orthopyroxenite and anorthosite samples from the Stillwater Complex (Montana) over peak pressures from 17 to 63 GPa. We acquired emissivity and hemispherical reflectance spectra (350–1400 cm−1; ∼7–29 μm) of both coherent chips and fine-grained powders of shocked and unshocked samples. These spectra are more directly comparable to remotely sensed data of Mars (e.g., TES) than previously acquired absorption or transmission spectra of shocked minerals. The spectra of experimentally shocked feldspar show systematic changes with increasing pressure due to depolymerization of the silica tetrahedra. For the spectra of chips, this includes the disappearance of small bands in the 500–650 cm−1 region and a strong band at 1115 cm−1, and changes in positions of a strong band near 940 cm−1 and the Christiansen feature near 1250 cm−1. Spectra of the shocked powders show the gradual disappearance of a transparency feature near 830 cm−1. Fewer changes are observed in the pyroxene spectra at pressures as high as 63 GPa. Spectra of experimentally shocked minerals will help identify more precisely the mineralogy of rocks and soils not only from TES but also from Mars instruments such as miniTES and THEMIS.

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Loreto G. FETTA, Appellant, v. NATIONSTAR MORTGAGE, LLC., Cypress Cove of Margate Homeowners Association, Inc., GE Money Bank f/k/a GE Capital Consumer Card Company, Oscar K. Johnson, as Successor Trustee for the Mary V. Blythe Revocable Trust Dated July 6, 1989, Appellees.

No. 4D17-2850

District Court of Appeal of Florida, Fourth District.

[June 28, 2018]

**DECISION WITHOUT PUBLISHED OPINION**

Affirmed.
Brett HABER, Appellant, v. Todd W. KLISTON, Appellee.

No. 4D17-3317

District Court of Appeal of Florida, Fourth District.

[June 28, 2018]

**DECISION WITHOUT PUBLISHED OPINION**

Affirmed.
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#           The thermophysical properties of the Bagnold Dunes, Mars: Ground truthing orbital data      

      May 30, 2018    

We compare the thermophysical properties and particle sizes derived from the Mars Science Laboratory rover's Ground Temperature Sensor of the Bagnold dunes, specifically Namib dune, to those derived orbitally from Thermal Emission Imaging System, ultimately linking these measurements to ground truth particle sizes determined from Mars Hand Lens Imager images. In general, we find that all three datasets report consistent particle sizes for the Bagnold dunes (~110–350 μm and are within measurement and model uncertainties), indicating that particle sizes of homogeneous materials inferred from temperature measurements and thermophysical models are reliable. Furthermore, we examine the effects of two physical characteristics that could influence the modeled thermal inertia and particle sizes, including (1) fine‐scale (centimeter to meter scale) ripples and (2) thin layering of indurated/armored materials. To first order, we find that small‐scale ripples and thin (approximately centimeter scale) layers do not significantly affect the determination of bulk thermal inertia from orbital thermal data using a single nighttime temperature. Modeling of a layer of coarse or indurated material reveals that a thin layer (< ~5 mm; similar to what was observed by the Curiosity rover) would not significantly change the observed thermal properties of the surface and would be dominated by the properties of the underlying material. Thermal inertia and particle sizes of relatively homogeneous materials derived from nighttime orbital data should be considered as reliable, as long as there are no significant subpixel anisothermality effects (e.g., lateral mixing of multiple thermophysically distinct materials).

## Citation Information

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                  -              Connect           

####             Kenneth Edward Herkenhoff, Ph.D. (Former Employee)          

##### Research Geologist

Astrogeology Science Center

## Related Content

####             Kenneth Edward Herkenhoff, Ph.D. (Former Employee)          

##### Research Geologist

Astrogeology Science Center

### Contact

####               Astrogeology Science Center          

2255 N. Gemini DriveFlagstaff, AZ86001United States

928-556-7000

928-556-7014

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                  - Bagnold Dunes
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<PAGE>

                                                                      EXHIBIT 32

         CERTIFICATE OF THE CHIEF EXECUTIVE AND CHIEF FINANCIAL OFFICER
           PURSUANT TO SECTION 906 OF THE SARBANES-OXLEY ACT OF 2002

      In connection with the annual report of Transition Auto Finance III (the
"Company") on Form 10-KSB for the year ended December 31, 2004, as filed with
the Securities and Exchange Commission on the date hereof (the "Report"), I,
Kenneth C. Lowe, the Chief Executive and Chief Financial Officer of the Company,
certify, pursuant to 18 U.S.C. Section 1350, as adopted pursuant to Section 906
of the Sarbanes-Oxley Act of 2002, that:

      1. The Report fully complies with the requirements of Section 13 (a) or 15
(d) of the Securities Exchange Act of 1934; and

      2. The information contained in this Report fairly presents, in all
material respects, the financial conditions and results of operations of the
Company.

Date: March 31, 2005                   s/ Kenneth C. Lowe
                                       ------------------
                                       Kenneth C. Lowe
                                   Chief Executive and Chief Financial Officer
----

CERTIFICATION PURSUANT TO  18 U.S.C. SECTION 1350,  AS ADOPTED PURSUANT TO  SECTION 906 OF THESARBANES-OXLEY ACT OF 2002 

 In connection with the Annual Report of Northport Investments,  Inc. (the “Company”) on Form 10-KSB for the period ending September  30, 2003, as filed with the Securities and Exchange Commission on the date hereof  (the “Report’), I, Stephen Dadson, Chief Executive Officer of the  Company, certify, pursuant to 18 U.S.C. Section 1350, as adopted pursuant to  Section 906 of the Sarbanes-Oxley Act of 2002, that:

|   | (1)    | The Report fully complies with the requirements of Section 13(a) or 15(d)      of the Securities Exchange Act of 1934; and                                        |
|--------|--------|-------------------------------------------------------------------------------------------------------------------------------------------------------------------|
|   |   |                                                                                                                                                              |
|   | (2)    | The information contained in the Report fairly presents,        in all material respects, the financial condition and result of operations        of the Company. |

| Dated: December 19, 2003 | By:    | /s/ Stephen Dadson                                           |
|--------------------------|--------|--------------------------------------------------------------|
|                     |   |    Steve Dadson  Chief Executive Officer |
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#           Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1976      

      January 1, 1976    

View Document

The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.

## Citation Information

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                  - United States
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114TH CONGRESS 

1ST SESSION H. R. 487 

AN ACT 

To allow the Miami Tribe of Oklahoma to lease or transfer 

certain lands. 

1 Be it enacted by the Senate and House of Representa2 tives of the United States of America in Congress assembled, 
2 

•HR 487 EH

1 SECTION 1. APPROVAL NOT REQUIRED TO VALIDATE LAND 

2 TRANSACTIONS. 

3 (a) IN GENERAL.—Notwithstanding any other provi4 sion of law, without further approval, ratification, or au5 thorization by the United States, the Miami Tribe of Okla6 homa may lease, sell, convey, warrant, or otherwise trans7 fer all or any part of its interests in any real property 

8 that is not held in trust by the United States for the ben9 efit of such tribe. 

10 (b) TRUST LAND NOT AFFECTED.—Nothing in this 

11 section shall— 

12 (1) authorize the Miami Tribe of Oklahoma to 

13 lease, sell, convey, warrant, or otherwise transfer all 

14 or any part of an interest in any real property that 

15 is held in trust by the United States for the benefit 

16 of such tribe; or 

17 (2) affect the operation of any law governing 

18 leasing, selling, conveying, warranting, or otherwise 

19 transferring any interest in such trust land. 

Passed the House of Representatives September 16, 

2015. 

Attest: 

Clerk. 

114TH CONGRESS 

1ST SESSION H. R. 487 

AN ACT 

To allow the Miami Tribe of Oklahoma to lease or 

transfer certain lands.
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#           SToRM:  A numerical model for environmental surface flows      

      January 1, 2009    

SToRM (System for Transport and River Modeling) is a numerical model developed to simulate free surface flows in complex environmental domains. It is based on the depth-averaged St. Venant equations, which are discretized using unstructured upwind finite volume methods, and contains both steady and unsteady solution techniques. This article provides a brief description of the numerical approach selected to discretize the governing equations in space and time, including important aspects of solving natural environmental flows, such as the wetting and drying algorithm. The presentation is illustrated with several application examples, covering both laboratory and natural river flow cases, which show the model’s ability to solve complex flow phenomena. 

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#           Predictive models for Escherichia coli concentrations at inland lake beaches and relationship of model variables to pathogen detection      

      February 21, 2013    

Predictive models, based on environmental and water quality variables, have been used to improve the timeliness and accuracy of recreational water quality assessments, but their effectiveness has not been studied in inland waters. Sampling at eight inland recreational lakes in Ohio was done in order to investigate using predictive models for Escherichia coli and to understand the links between E. coli concentrations, predictive variables, and pathogens. Based upon results from 21 beach sites, models were developed for 13 sites, and the most predictive variables were rainfall, wind direction and speed, turbidity, and water temperature. Models were not developed at sites where the E. coli standard was seldom exceeded. Models were validated at nine sites during an independent year. At three sites, the model resulted in increased correct responses, sensitivities, and specificities compared to use of the previous day's E. coli concentration (the current method). Drought conditions during the validation year precluded being able to adequately assess model performance at most of the other sites. Cryptosporidium, adenovirus, eaeA (E. coli), ipaH (Shigella), and spvC (Salmonella) were found in at least 20% of samples collected for pathogens at five sites. The presence or absence of the three bacterial genes was related to some of the model variables but was not consistently related to E. coli concentrations. Predictive models were not effective at all inland lake sites; however, their use at two lakes with high swimmer densities will provide better estimates of public health risk than current methods and will be a valuable resource for beach managers and the public.

## Citation Information

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                  -              Connect           

####             Donna Francy (Former Employee)          

##### Hydrologist  (Water Quality Specialist)

Ohio-Kentucky-Indiana Water Science Center

#### Erin A Stelzer

##### Microbiologist

Ohio-Kentucky-Indiana Water Science Center

eastelzer@usgs.gov

614-516-1188

#### Joe Duris

##### Water Quality Specialist - Microbiologist

Pennsylvania Water Science Center

jwduris@usgs.gov

717-730-6930

## Related Content

####             Donna Francy (Former Employee)          

##### Hydrologist  (Water Quality Specialist)

Ohio-Kentucky-Indiana Water Science Center

#### Erin A Stelzer

##### Microbiologist

Ohio-Kentucky-Indiana Water Science Center

eastelzer@usgs.gov

614-516-1188

#### Joe Duris

##### Water Quality Specialist - Microbiologist

Pennsylvania Water Science Center

jwduris@usgs.gov

717-730-6930

### Study Area

### Contact

####             Water Resources Mission Area - Headquarters        

USGS Headquarters12201 Sunrise Valley DriveReston, VA20192United States

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                  - United States
                  - Ohio

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#           Sand-calcite crystals from Garfield County, Utah      

      January 1, 1984    

View Report

Sand-calcite crystals are found in the Morrison Formation of Jurassic age in south-central Garfield County, Utah. The outcrop area is less than 1 acre, yet the locality contains many fine specimens of single, double, and complex crystals in good hexagonal form. This is the first known occurrence of sand-calcite crystals in rocks of Jurassic age and is the first reported occurrence in Utah.

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                  - Utah

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#           Resources for teachers and students at the Upper Midwest Environmental Sciences Center      

      January 1, 2004    

No abstract available.

## Citation Information
This section of the FEDERAL REGISTER

contains editorial corrections of previously

published Presidential, Rule, Proposed Rule,

and Notice documents. These corrections are

prepared by the Office of the Federal

Register. Agency prepared corrections are

issued as signed documents and appear in

the appropriate document categories

elsewhere in the issue.

Corrections Federal Register

58924

Vol. 61, No. 224

Tuesday, November 19, 1996

SECURITIES AND EXCHANGE

COMMISSION

[Release No. 34-37890; File Nos. SR-Amex96-37, SR-NYSE-96-30, and SR-Phlx-96-43]

Self-Regulatory Organizations; Notice

of Filing and Order Granting

Accelerated Approval of Proposed

Rule Changes by the American Stock

Exchange, Inc., New York Stock

Exchange, Inc., and Philadelphia Stock

Exchange, Inc. Relating to an

Extension of Certain Market-Wide

Circuit Breaker Provisions

Correction

In notice document 96–28385

beginning on page 56983 in the issue of

Tuesday, November 5, 1996, make the

following correction:

On page 56985, in the third column,

above the FR Doc. line, the signature

was omitted and should read as set forth

below:

Margaret H. McFarland,

Deputy Secretary.

BILLING CODE 1505–01–D

SECURITIES AND EXCHANGE

COMMISSION

[Release No. 34-37846; File No. SRPhiladep-96-13]

Self-Regulatory Organizations;

Philadelphia Depository Trust

Company; Order Granting Permanant

Approval of Proposed Rule Change

Concerning Procedures Relating to

Rule 17Ad-16

Correction

In notice document 96–27527

beginning on page 55679 in the issue of

Monday, October 28, 1996 make the

following correction:

On page 55680, in the second column,

above the FR Doc. line, the signature

was omitted and should read as set forth

below:

Margaret H. McFarland,

Deputy Secretary.

BILLING CODE 1505–01–D

DEPARTMENT OF TRANSPORTATION

Federal Aviation Administration

14 CFR Part 121

[Docket No. 27218; Amendment 121-261]

RIN 2120-AD74

Protective Breathing Equipment;

Correction

Correction

In rule document 96–27991 appearing

on page 57858 in the issue of Thursday,

November 7, 1996, in the first column,

in the second line from the bottom,

‘‘(b)(9)(iii)’’ should read ‘‘(b)(7)(iii)’’.

BILLING CODE 1505–01–D
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#           Recharge of the early atmosphere of Mars by impact-induced release of CO2      

      January 1, 1989    

Channels on the Martian surface suggest that Mars had an early, relatively thick atmosphere. If the atmosphere was thick enough for water to be stable at the surface, CO2 in the atmosphere would have been fixed as carbonates on a relatively short time scale, previously estimated to be 1 bar every 107 years. This loss must have been offset by some replenishment mechanism to account for the numerous valley networks in the oldest surviving terrains. Impacts could have released CO2 into the atmosphere by burial, by shock-induced release during impact events, and by addition of carbon to Mars from the impacting bolides. Depending on the relationship between the transient cavity diameter and the diameter of the resulting crater, burial rates as a result of impact gardening at the end of heavy bombardment are estimated to range from 20 to 45 m/106 years, on the assumption that cratering rates in Mars were similar to those of the Nectarian Period on the Moon. At these rates 0.1-0.2 bar of CO2 could have been released every 107 years as a result of burial to depths where dissociation temperatures of carbonates were reached. Modeling of large impacts suggests that an additional 0.01 to 0.02 bar of CO2 could have been released every 107 years during the actual impacts. In the unlikely event that all the impacting material was composed of carbonaceous chondrites, a further 0.3 bar of CO2 could have been added to the atmosphere every 107 years by oxidation of meteoritic carbon. Even when supplemented by the volcanically induced release of CO2, these release rates are barely sufficient to sustain an early atmosphere if water were continuously present at the surface. The results suggest that water may have been only intermittently present on the surface early in the planet's history.

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#           Putting down roots in earthquake country: Your handbook for the San Francisco Bay region      

      September 13, 2005    

View Document

This handbook provides information about the threat posed by earthquakes in the San Francisco Bay region and explains how you can prepare for, survive, and recover from these inevitable events. If you live or work in the region, you need to know why you should be concerned with earthquakes, what you can expect during and after a quake, and what you need to do beforehand to be safe and reduce damage.

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                  - United States
                  - San Francisco Bay
                  - california

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#           Significance of stress transfer in time-dependent earthquake probability calculations      

      January 1, 2005    

A sudden change in stress is seen to modify earthquake rates, but should it also revise earthquake probability? Data used to derive input parameters permits an array of forecasts; so how large a static stress change is require to cause a statistically significant earthquake probability change? To answer that question, effects of parameter and philosophical choices are examined through all phases of sample calculations, Drawing at random from distributions of recurrence-aperiodicity pairs identifies many that recreate long paleoseismic and historic earthquake catalogs. Probability density funtions built from the recurrence-aperiodicity pairs give the range of possible earthquake forecasts under a point process renewal model. Consequences of choices made in stress transfer calculations, such as different slip models, fault rake, dip, and friction are, tracked. For interactions among large faults, calculated peak stress changes may be localized, with most of the receiving fault area changed less than the mean. Thus, to avoid overstating probability change on segments, stress change values should be drawn from a distribution reflecting the spatial pattern rather than using the segment mean. Disparity resulting from interaction probability methodology is also examined. For a fault with a well-understood earthquake history, a minimum stress change to stressing rate ratio of 10:1 to 20:1 is required to significantly skew probabilities with >80-85% confidence. That ratio must be closer to 50:1 to exceed 90-95% confidence levels. Thus revision to earthquake probability is achievable when a perturbing event is very close to the fault in question or the tectonic stressing rate is low.

## Citation Information
Exhibit 32.2

Certification Pursuant to Section 906 of the Sarbanes-Oxley Act of 2002

Pursuant to 18 U.S.C. §1350, I, the undersigned Chief Financial Officer of Witness Systems, Inc. (the "Company"), hereby certify to my
knowledge and belief that the Quarterly Report on Form 10-Q of the Company for the quarterly period ended September 30, 2003 (the "Report") fully complies with the
requirements of Section 13(a) of the Securities Exchange Act of 1934 and that information contained in the Report fairly presents, in all material respects, the financial condition and results
of operations of the Company.

Dated:
November 13, 2003

| |  | BY: |  | /s/WILLIAM F. EVANSWilliam F. Evans Chief Financial
Officer
| |  | --- |  | -----------------------------------------------------------



A
signed original of this written statement required by Section 906, or other document authenticating, acknowledging, or otherwise adopting the signature that appears in typed form within the
electronic version of this written statement required by Section 906, has been provided to Witness Systems, Inc. and will be retained by Witness Systems, Inc. and furnished to the
Securities and Exchange Commission or its staff upon request.

45

---

QuickLinks
Mariam MARTIBENNING, Appellant/Petitioner(s), v. Chad CHRONISTER, Sheriff of Hillsborough County, Florida, Appellee/Respondent(s).

CASE NO.: 2D18-1592

District Court of Appeal of Florida, Second District.

May 09, 2018

**DECISION WITHOUT PUBLISHED OPINION**

Granted.
J.L.S., A Child, Appellant, v. STATE of Florida, Appellee.

Case No. 5D17-3948

District Court of Appeal of Florida, Fifth District.

Decision filed June 19, 2018

**DECISION WITHOUT PUBLISHED OPINION**

AFFIRMED.