2013 Texas Wildlife and Woodland Expo

On Saturday thousands of visitors descended on the Lone Star College-Montgomery Campus in Conroe to learn about the forests of the region in which they live and how to best take care of it through hands on clinics, information booths, live demonstrations, and children's activities.  Attendees ranged from urban homeowners to rural landowners, boy scouts, girl scouts, outdoor enthusiasts and everyone in between.

Donna Work explains the importance of streamside management zones using the SMZ simulator

Hughes Simpson discusses benthic samples with visitors

The Water Resources program was on hand to answer questions related to water resources and provide information on forestry BMPs.  Donna Work, Hughes Simpson, and Todd Thomas handed out information and discussed BMPs and the forest-water relationship to any interested patrons of the event.  A demonstration was on hand to illustrate the importance of maintaining Streamside Management Zones (SMZs) complete with rainfall and runoff simulation.

Todd Thomas talks BMPs with expo enthusiasts 

SFA Students Experience BMPs Firsthand

Last week, 46 students enrolled in ecology at Stephen F. Austin State University were able to view various Texas forestry best management practices (BMPs) implemented on the ground in northeast Nacogdoches County.  In addition to viewing methods of erosion control in forestry operations, the students learned about various facets of the program including the effectiveness monitoring project.  While learning about the BMP effectiveness project, the students were able to view equipment used to sample benthic organisms, as well as some organisms that were living in the creek running through the tract.

Biologist Donna Work discusses benthic macroinvertebrates 

March 2013 BMP Q&A

By: Todd Thomas, Water Resources Forester, Texas A&M Forest Service

Q:  I was looking at a Texas BMP compliance monitoring checklist and in the comments section, it mentioned “below grade roads”.  I have heard this term mentioned before, but I have never been quite sure what a below grade road is and what exactly can I do about them?

A: I am glad you asked this.  A road that is below grade is one that is lower than the surrounding land.  Many of the roads in East Texas are very old and can be classified as below grade. 

Below grade roads usually occur after years of being worked and graded without any new material brought in to build them up, or from just being worked from one direction, to the point that the road essentially becomes a channel for runoff water.  As you may remember, with BMPs we are trying to keep from channelizing any runoff.  When runoff is channeled it begins to accelerate, especially in areas with a great deal of topography.  This accelerated runoff will increase erosion and the amount of sediment that reaches our streams. 

The issue of below grade roads is not limited to areas with rolling terrain or steep topography, below grade roads can create significant problems in flatwoods as well.  The issue isn’t so much a concern with water quality, but with access.  Water will always flow to the lowest spot on a site, and if this happens to be the roadway, then the water will not properly drain.  The road will then become saturated, and stay wet for most of the year.  Wet roads can lead to poor access, and cause severe rutting if traveled. 

These situations can develop gradually over time if roads are not properly constructed or may occur when subjected to heavy rains.  The formation of these areas can also result from trying to access a wet road by cutting it down until a dry surface is reached.  While this might be a temporary solution to an access problem, it can lead to erosion problems. 

To fix or reduce the severity of these problems, the first thing you need to decide is if the road in question will function as a temporary or permanent road.  This can be dictated by the amount of traffic your road will handle in the near future.  High traffic zones will generally be more expensive to control than low traffic zones.   If the road is not necessary then it should be closed.  In order for the road to stay in use the surface will need to be built up and water control structures will need to be put into place.  The type of structure will be dictated by the traffic type.  

There are several effective ways to reduce the impact to water quality on below grade roads.  It is best to make sure that the roadway is well drained when dealing with permanent systems located on steep topography.  Installing waterbars with good outlets for the water is recommended.  Instead of using the dirt in the roadway to build these structures, try incorporating some of the bank dirt.  This will allow you to construct a waterbar and at the same time make it easier to divert the water. 

When dealing with temporary roads, revegetating is a great option to hold the soil in place and minimize the amount of erosion and sedimentation that may occur.  A more cost efficient way to hold temporary roads in place is to distribute fine slash on the roadbed.  If you have any questions about BMPs, please do not hesitate to contact me at (936) 639-8180 or email me at tthomas@tfs.tamu.edu.  

*This article was published in the March 2013 edition of the Texas Logger

February 2013, BMP Q&A

By: Todd Thomas, Water Resources Forester, Texas A&M Forest Service

Q: In the quiz last month you asked a question where we would need to know the slope in order to have appropriately spaced windrows.  My question is how are we supposed to know the slope in the field off hand without a tool such as a clinometer? 

A: I am glad you asked this question and I am always glad to highlight areas of the blue book.  However this time I will not be referencing the text of the book, but a feature that many of you may have noticed, but never paid much attention to.  This feature is the slope calculator. 

The slope calculator can be found on the inside of the back cover of the blue book.  There are instructions on how to use it, but since you asked, I will go ahead and explain.  In addition to your blue book, you will need a piece of string, approximately 12-inches long and something to use as a weight, such as a small nut or washer.  First, tie one end of the string to the middle ring of the spiral binding or punch a hole through the cover of the book at the apex of the slope calculator.  Go ahead, it is okay.  There is a small circle there for your reference.  Next, tie your small weight to the loose end of the string. 

Now that your slope calculator has been constructed, here is how you will use it.  The spiral binding should be on top, use this as your sight.  With the binding parallel to the ground, sight the book up or down the slope (depending on which way you are facing), the string will hang vertically and the slope can be read directly along the line where the string lies.  The number on the line with the string is your percent slope.

Now that you are aware of the slope calculator, there are no excuses for not having your blue book with you.  Not only is the book full of BMP information, it is also a tool that you can use in your day to day functions.  In addition to windrow spacing, this tool can be used for determining road gradients so you know where to locate your water control structures such as waterbars, wing ditches, culverts, and dips; in conjunction with the culvert size chart to determine culvert sizing; as well as how wide to make SMZs when near steep slopes, or any other time you need to know the percent slope in a pinch. 

In conclusion, keep those blue books handy, you never know when one might come into use.  If you need a blue book you can get one from your nearest TFS office.  Please keep your questions coming.  You can email them to me at tthomas@tfs.tamu.edu or phone them in by calling (936)639-8180.  

*This article was published in the February 2013 issue of the Texas Logger

December 2012 BMP Q&A

By: Todd Thomas, Water Resources Forester, Texas A&M Forest Service

Q: Awhile back I noticed on some closed out skid trails that had been revegetated, not only was rye grass used, but they had also used some clover in the mix.  Is there any benefit to planting clover when in areas that you are revegetating?

Revegetated Logging Road, East Texas

A: I am always glad to hear about revegetation, as it is an excellent method of preventing erosion on roads and other disturbed areas.  It is even better to hear of the clover being used in the mix.  This is because clover is a type of plant that is also known as a “legume”.  Legumes can be important in areas where there has been a considerable amount of soil disturbance such as a skid trail or approach to a stream crossing. 

Legumes perform what is called nitrogen fixation.  In other words, they take nitrogen from the air and put it back into the soil.  Nitrogen is an extremely important nutrient for plant growth.  This is why sometimes in agricultural operations you will see peanuts or soybeans used in crop rotation, since they can contribute nitrogen back to the soil that was depleted by the previous crop.  In an area with a great deal of disturbance it is important to incorporate something in your revegetation that can contribute back to the soil not only by helping to hold it in place, but by delivering a much needed nutrient that will help other grasses to grow, further preventing erosion. 

Subterranean clover

On page 66 of the blue book, it says that “legumes should be used in mixes with grasses.”  On the next page it gives some options for different legumes to use.  The legumes that we recommend incorporating are Singletary peas, Hairy vetch, Arrowleaf clover, and Subterranean clover.  However, if you choose to incorporate another legume, that is great also.  In general, all clovers, as well as plants that have some sort of seed pod (such as peas or beans) are legumes. 

A side benefit of planting legumes is that they are a great food source for wildlife.  Most legumes are high in protein, and all our deer hunters out there know that additional protein can increase antler growth in whitetail deer.  I’m sure the landowner will be extra happy knowing that you have helped their quest for “Muy Grande”.  This is just a side benefit while you are doing an excellent job at rebuilding soil productivity and reducing erosion. 

So remember to always include legumes in your revegetation and to keep the questions coming.  You can email me your questions at tthomas@tfs.tamu.edu or by phone at (936)639-8180.  Also, be sure to pay a visit to our blog at http://tfswater.blogspot.com.  On the blog you can find old Q&A articles, as well as additional information on how to best keep our waters clean while providing the world with forest products.  

*This article was published in the December 2012 issue of the Texas Logger

November 2012 BMP Q&A

By: Todd Thomas, Water Resources Forester, Texas A&M Forest Service

Q: Just the other day, the topic of temporary stream crossings came up.  More specifically, how does TFS recommend that we cross streams and how should they be left after operations are complete on the site? 

A:  Excellent question, if you don’t give proper care and thought to your temporary stream crossings, many of the BMPs you have put into place on the tract can be negated.  A key component of any forest management activity is access.  In some cases you may not have to cross streams to access parts of a tract that you need to.  For instance, there may be another entrance or road that has been overlooked, a neighboring landowner may grant access through their property, or it may not be necessary at all once you have stepped back and looked at the bigger picture. 

More often than not, you are going to have to put in a stream crossing or two to get the job done, but remember to keep them to a minimum.  When selecting a location be sure and look for a straight, narrow section of stream with relatively low banks.  This will minimize the amount of disturbance to the stream and stream banks.  Higher banks result in a greater amount of disturbance than lower banks, and straight, narrow sections limit the amount of exposure the streambed receives from equipment.  Once you have selected the appropriate location, be sure that your approaches to the stream as well as the crossing itself is at a 90 degree angle to the stream, this ensures that as equipment crosses, the amount of the stream exposed to equipment is greatly reduced. 

Log skidder dragging logs across a temporary bridgemat

If the banks of the stream are too high for equipment to cross directly, a common approach is to lay slash bundles into the stream bed that can be driven across.  The only downside to this is that they must be removed following operations; this can take some effort and can result in a serious amount of disturbance.  However, this is a much better option than dirt crossings.  Dirt crossings should never be used and are never recommended.  Remember, the point of BMPs is to keep extra dirt from entering the streams, not to add any more.  One of the easiest alternatives for these types of crossings is to use bridgemats, otherwise known as skidder mats or dragline mats.  These mats are constructed of hardwood cants that have been bolted together and are extremely durable and can be used over and over again.  They can be laid in place with the grapples of the skidder and removed in the same fashion once you are done.  The best part is that you have stayed out of the stream bed completely and maximized water quality protection at your temporary stream crossing. 

Once it is time to move off site, temporary stream crossings should be removed and the approaches should be stabilized to reduce erosion.  One way to stabilize approaches is by revegetating them.  On page 65 of the most recent BMP handbook there are guidelines for revegetating disturbed areas, there is even a chart that gives you different seeding options so that you can use the best seed for your site.  Another alternative is to distribute fine slash down the approach (being sure not to put any in the stream bed) and drive over it to ensure firm placement, followed by larger, more coarse slash. 

In conclusion, remember to keep stream crossings to a minimum, always stabilize your approaches and to never use dirt crossings.   Keep the questions coming so we can shed some light on any best management practice confusion that might be out there, you can send your questions to me at tthomas@tfs.tamu.edu or just phone it in by calling (936) 639-8180.

*This article was published in the November 2012 issue of the Texas Logger

Polk County Landowner Meeting

On Saturday, October 27, Texas A&M Forest Service personnel helped to put on a meeting in Livingston, Texas for landowners in Polk County.  The meeting was sponsored by the Sustainable Forestry Initiative (SFI) and the Texas Forestry Association.  60 landowners showed up to increase their knowledge of sound forest management and issues surrounding modern forestry.

The topics and speakers included

• The Sustainable Forestry Initiative (SFI)
• Steve Mayo, MeadWestvaco
• East Texas Land Sales and Acquisitions
• Wes Kilpatrick, Walsh Land Brokers
• Legislative Update
• Ron Hufford, Texas Forestry Association
• Woodville Renewable Power Project
• Ryan Thomas, East Texas Electric Cooperative, Inc. 
• Multiple Use Forestry
• Gary Burns, Burns Forestry
• Lonleaf Pine: Past, Present, and Future
• Jared Goodman, Texas A&M Forest Service
• BMPs: What You Should Know as a Forest Landowner
• Todd Thomas, Texas A&M Forest Service

Not only was it a good learning experience for forest landowners, it was an opportunity for many of them to become acquainted with one another as well as for the Polk County Landowner Association to boost their membership.  Landowner associations play in an integral role in landowner education, ensuring that the members are aware of current issues and sound forest management.